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INTERNATIONAL SOCIETY FOR
SOIL MECHANICS AND
GEOTECHNICAL ENGINEERING
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the International Society for Soil Mechanics and
Geotechnical Engineering (ISSMGE). The library is
available here:
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g- Norwegian Geotechnical Institute (NGI) and University of Oslo, Norway
ABSTRACT: The safety and performance of adamis inseparable fromthe capacity of its foundation. A briefreview is made of Ter-
zaghi’s involvement in embankment dams. The lessons learned and the state of the art are discussed together with statistics on dam
incidents and failures. The safety record for tailing dams is not satisfactory and must be improved by getting more damengineering
know-how into the design and construction of these types of structures. The principle of designing to provide defence in depth with
“belt and suspenders (braces)” is an essential consideration. The tasks of performing safety evaluation, risk analysis and remediation
of ageing dams are as challenging as the original damdesign and construction. In addition to required rehabilitation, many dams re­
quire upgrading to resist higher flood levels, stronger earthquakes and more stringent safety criteria than those applied at the time of
design and construction. The paper concludes by emphasizing the need for safety legislation, damengineering education, and careful
planning ofdams to support sustainable development.
RÉSUMÉ: La sécurité et le comportement d'un barrage est inséparable de la capacité de sa fondation. L'article fait d'abord un court
résumé des travaux de Terzaghi sur les barrages en remblai, discute les leçons importantes apprises et l'état de l'art aujourd'hui et pré­
sente quelques statistiques sur les incidents et ruptures de barrages. Les barrages bâtis avec résidus miniers n'ont pas uncomportement
satisfaisant aujourd'hui. Ces barrages peuvent être améliorés par l'introduction du savoir-faire de l'ingénieur dès leur conception et
construction. Une conception avec le principe “belt and suspenders (braces)”est essentielle. L'évaluation de la sécurité, les analyses
de risque et la rénovation des barrages anciens présentent les mêmes défis que leur conception initiale. En plus de la réhabilitation,
plusieurs barrages requièrent une amélioration pour pareràdes crues plus élevées, des séismes plus violents et des critères de sécurité
plus sévères qu'initialement. L'article termine sur une perspective d'urgents besoins: législation sur la sécurité, éducation plus étendue
sur l'ingénierie des barrages et planification attentive des barrages étayant un développement durable et responsable de l'environne­
ment.
1 INTRODUCTION
The planning, design and construction of an embankment dam
represents one of the most challenging and exciting endeavours
in the field of geotechnical engineering. World-wide there are
approximately 30,000 large embankment dams higher than 15 m
(ICOLD, 1998). They are of many different designs and rest on
foundations varying fromproblem-free, virtually impervious and
incompressible bedrock to geologically complex, stratified, com­
pressible, weak and pervious soil deposits. Several of them are
built on pre-existinglandslides (Schuster, 2000).
More than half of the dams, and by far the biggest ones, are
built since 1950. However, many are more than 100 years old.
The safety re-evaluation and possible strengthening of existing
dams and their foundations is a challenge no less demanding
than the original design and construction work. The dams were
built at a time when the state of the art, based on field experi­
ence, performance observations, and geotechnical analyses, was
much inferior to current level of understanding of embankment
and foundation behaviour. Furthermore, the safety re-evaluation
is made even more difficult by lack of adequate documentation
of the original site investigation, foundation treatment, damde­
sign andconstruction.
Table 1gives alisting of the highest dams inexistence. There
are 10 embankment dams, all built during recent years, higher
than 210 m, but 65% of all large dams registered are less than
30 m high. The highest dams may not necessarily have repre­
sented the most challenging ones as the foundation andabutment
conditions, the seismicity of the region, and the availability of
suitable embankment construction materials significantly influ­
ence the degree of difficulty in achieving asuccessful result. The
safety and performance of adamis inseparable fromthecapacity
ofits foundation.
Table 1. World’s highest dams
Name Country Height
(m)
Dam type
Rogun Tadjikistan 335 Embankment *
Nurek Tadjikistan 330 Embankment
Grande Dixence Switzerland 285 Concrete (arch)
Inquiry Georgia 272 Concrete (arch)
Vajont Italy 261 Concrete (arch)
Manuel M. Tones Mexico 261 Embankment
Alvaro Obregon Mexico 260 Concrete (gravity)
Mauvoisin Switzerland 250 Concrete (arch)
Mica Canada 243 Embankment
Alberto Lleras C. Colombia 243 Embankment
Sayano- Russia 242 Concrete (arch)
Shushenskaya
Ertan China 240 Concrete (arch)
La Esmaralda Colombia 237 Embankment
Kishau India 236 Concrete (gravity)
Oroville USA 235 Embankment
*underconstruction
The following presentationis given under the headings:
• Terzaghi andembankment dams
• State ofthe art
• Statistics on damincidents andfailures
• Performance evaluation, safety assessment andremediation
• Systematic riskanalyses
• The need fordamsafety legislation and damengineering edu­
cation
• The debate about dams andsustainable development
2491
2 TERZAGHI AND EMBANKMENTDAMS
There is little mention of embankment dams as such in Ter-
zaghi’s classical and remarkable book “Erdbaumechanik auf
bodenphysikalischer GrundlageT, written here in Istanbul in
1924. In the last article entitled “Earth as building material”, he
briefly discusses hydraulic fill dams, the grain size distribution
in the core, the compaction of the core material andthe analyses
of stresses in the core. Terzaghi was early very much aware of
the possibility of soil erosion leading to piping, which was
among the first subjects of his experimental investigations at
Robert College inIstanbul. Already in 1922 he hadpublished his
findings and secured a patent on inverted filters for the protec­
tion against failure by piping in soil foundations for concrete
dams.
During the following years Terzaghi recognized more and
more clearly that the safety of dam foundations with respect to
piping depends to a large extent on minor geological details of
the subsoil, and in 1929 he published his by now classic paper
“Effect of minor geological details on the safety of dams”. T
T
iis
contribution highlighted the uncertainties that are an essential
part of geotechnical practice and, as noted by Terzaghi (1961),
led to the articulation of the observational method, a philosophy
andprocedure elegantly expanded upon by Peck (1969).
Terzaghi considered the design of the embankment portion of
the dams aproblemof secondary importance. He believed that if
the subsoil conditions and the pattern of seepage were reliably
known in advance of construction, the stability problems could
usually be solved with adequate approximation by theory, on the
basis of theresults of laboratorytests (Bjerrumet al., 1960). This
attitude is reflected in his selection of projects on which he co­
operated. During his professional career he was associated with
the design, or with the design andconstruction ofabout 30 earth-
or rockfill dams. Practically all these dams, except the earliest
ones, are located on subsoils with an erratic pattern of stratifica­
tion, precluding areliable forecast of the pattern of seepage prior
to construction. The Vermilion Dam, California (Terzaghi and
Leps, 1958), the Cheakamus Dam, British Columbia (Bjerrumet
al, 1960), and the Mission Dam, British Columbia (Terzaghi and
Lacroix, 1964) are representative of the types of projects that
aroused Terzaghi’s interest. The reading of these papers is a
must for adamengineer.
In the first edition of “Soil Mechanics in Engineering Prac­
tice” (Terzaghi and Peck, 1948) there is a chapter on dams with
much emphasis on damfoundations and the danger of piping. In
the preface to the second edition, which appeared in 1967 four
years after Terzaghi’s death, Peck writes that Terzaghi had
“added extensively to the articles on dams and their foundation.
Since dams occupied an increasingly larger portion of his activi­
ties during his lateryears, these additions maybe regarded as the
essence of his experience andthoughts on the subject.”
The introduction to the third edition of “Soil Mechanics in
Engineering Practice” (Terzaghi, Peck and Mesri, 1996), says
that: ”...every statement and conclusion, pertaining to soils in
the field involves many uncertainties. In extreme cases the con­
cepts on which adesign is based areno more thancrude working
hypotheses that may be far fromthe truth. In such cases the risk
of partial or total failure can be eliminated only by using what
may be called the observational procedure. This procedure con­
sists of making appropriate observations soon enough during
construction to detect any signs of departure of the real condi­
tions from those assumed by the designer and of modifying ei­
ther the design or the method of construction in accordance with
the findings.”
The engineeringjobs that tested Terzaghi’s insight in his ma­
ture years were mainly the water and power projects in the gla­
ciated mountains of California, and especially British Columbia
(Goodman, 1999). Terzaghi is quoted as saying that the design
and construction of Mission Dam was the most difficult and
most daring engineering project of his entire career (Casagrande,
1964). The site is underlain by two very pervious aquifers, and
underthe major portion of the damthese are separated by athick
stratumof weak and highly compressible clay. Adeep grout cur­
tain through the lower aquifer, extending to amaximumdepth of
about 170 m, and a sheet pile cut-off through the upper aquifer
control seepage through the foundation. The nature of the avail­
able construction materials and the anticipated large differential
settlements (up to 5 m) led to the design of a zoned type of em­
bankment dam. The low shear resistance of the clay stratumre­
quired that the damhave a very gentle upstreamslope. The high
compressibility of the clay stratum made it necessary to design
the damin such a way that the highest portion would be under­
lainonly by coarse-grained sediments in order to avoid excessive
settlement of that portion. The dam incorporates the very first
major use of a plastic membrane (geomembrane) over a portion
of the clay blanket on the upstreamslope. The membrane, which
lies under a protective cover of earth fill, was put in as an extra
line of defence in case the clay blanket should crack due to ex­
cessive differential settlements.
The design, construction and surveillance of Mission Dam
turned out to be Terzaghi’s last job, and the famous paper by
Terzaghi and Lacroix (1964) was published after his death with
the assistance of careful reviews by his wife Ruth Terzaghi and
Arthur Casagrande. At a special session in memory of Terzaghi
that opened the Sixth International Conference on Soil Mechan­
ics and Foundation Engineering, Montreal (1965), the British
Columbia Hydro and Power Authority renamed Mission Dam
theTerzaghi Dam.
3 STATEOFTHEART
It is not the ambition of this contribution to give a comprehen­
sive review of the state of the art of the engineering of embank­
ment dams and their foundations. Only a few aspects will be
touched upon in the following sections pointing to challenges in
the years to come. However, some of the more important general
literature references are singled out and listed below.
ICOLD (International Commission on Large Dams) was
founded already in 1928 and organizes aworld congress every 3
years. For each congress four specific topics (questions) are se­
lected for discussion resulting indetailed proceedings, usually in
five separate volumes. In addition, ICOLD publishes each year
several bulletins (state-of-the-art guidelines) based on the work
inICOLD’s manytechnical and special committees.
A limited number of textbooks exist, andthere are some valu­
able books compiled from contributions at workshops and spe­
cial symposia (complete information in reference list):
• Sherardet al., 1963 “EarthandEarth-RockDams”.
• Hirschfeld and Poulos (editors), 1973 “Embankment-Dam
Engineering”Casagrande Volume.
• US National Research Council, 1983 “Safety of Existing
Dams".
• Cooke and Sherard (editors), 1985 “Concrete Face Rockfill
Dams”.
• Leonards (editor), 1987 “DamFailures".
• Jansen (editor), 1988 “Advanced DamEngineering”.
• Neves (editor), 1991 “Advances in Rockfill Structures”.
• Kjæmsli et al., 1992 “Rockfill Dams - Design and Construc­
tion”.
• Fell, MacGregor and Stapledon, 1992 “Geotechnical Engi­
neering of Embankment Dams”.
• Singh and Varshney, 1995 “Engineering of Embankment
Dams”.
• Terzaghi, Peck and Mesri, 1996 “Soil Mechanics in Engi­
neeringPractice”.
It should be noted that in several of thebooks listed above by
the names of their editors, there are excellent contributions
(chapters) by some of the outstandingengineers in the field.
T
T
ie central role of the topic of embankment dams and their
foundations in geotechnical engineering is demonstrated by the
many Rankine and Terzaghi lectures on various aspects of the
2492
subject (e.g. Casagrande, 1961; Newmark, 1965; de Mello, 1977;
Seed, 1979; Cook, 1984; Penman, 1986). RalphPeck presenteda
lecture in 1979, which he entitled “Where has all thejudgement
gone”(Peck, 1980). Since then he has repeatedlyreturnedtothis
theme, and below is anexcerpt fromthat paper; mainly referring
toembankment dams:
.... A failure is seldom the consequence of a single short­
coming. Usually there is at least one other defect or deficiency,
and the failure occurs where two or more coincide. This infer­
ence supports the principle of designing to provide defence in
depth, the “belt and suspenders”principle long advocated by Ar­
thur Casagrande. It postulates that if any defensive element in
the damor its foundation should fail to serve its function, there
must be one or more additional defensive measures to take its
place. Teton Dam is an outstanding example of violation of the
principle; the sole line of defence was the core andgrout curtain.
Under such conditions, it is almost irrelevant to define the pre­
cise manner in which the failure started or whether there may
have been such deficiencies in construction as awet seamacross
the core. The design should have provided adequate defences
against anysuch defect.
The bedrock treatment appropriate to the geological condi­
tions is amatter of design. It is not an aspect of design suscepti­
ble, however, to numerical analysis. Instead, it requires the exer­
cise ofjudgement, a sense of proportion. Whenjointed bedrock
foundation is being treated and covered with the first layers of
fill - acrucial time with respect to the future performance of the
dam- engineers fully acquainted with the design requirements
should be present, should have the authority to make decisions
on the spot, and should not delegate their authority unless and
until they are satisfied that theirjudgement concerning the par­
ticular project has been fully appreciated by their subordinates.
I doubt if guidelines, regulations, or even the best of specifi­
cations can take the place of personal interaction between de­
signers and field forces at his stage. Frequently, as a consultant
or as a member of a board of consultants, I have walked over a
recently exposed foundation or abutment with the field forces,
discussing place by place what treatment would be appropriate.
Together we studied details of foundation conditions, observed
treatment in progress, agreed upon orchanged it. Inthis manner,
the consultants evaluated the potential problems and their solu­
tions, and the field forces gained the necessary insight as to what
was required.
The type of foundation treatment is not a matter to be deter­
mined by ageologist, unless he is truly anengineering geologist.
The geologist should investigate the geological characteristics of
the foundation and its interface with the dam and make them
known to the engineer who will form thejudgement concerning
treatment. The consequences of the flow of water near the inter­
face, including its effect on the various materials in the dam, are
within the realm of the engineer and the decisions regarding
treatment areengineeringdecisions.
The three failures that I have discussed in some detail origi­
nated at the interface between dam and foundation. Others, that
might equally have been chosen as examples, arose from over­
looking or misjudging geological features in the foundation it­
self. A few had their origin in construction defects in the em­
bankment. They had in common that all were outside the scope
of numerical analyses. They would have been prevented if
judgement arising fromextensive experience had been given full
scope of design and construction, and if the design hadincluded
multiple defences. Accordingly, I think it quite possible that the
incidence of failure of major dams could be reduced an order of
magnitude by focusing attention on the details of design and
construction that cannot, at least presently, be covered by analy­
sis, that perhaps cannot beknown until construction is underway,
but that require the personal attention of experienced engineers.
Research should be directed to those aspects of design and con­
struction in greatest need of improvement; definition of founda­
tionconditions; conditions conducive to internal erosion and the
means for controlling it; filter criteria and their practical
achievement in construction; prevention and treatment of crack­
ing. The goal of the research should be improved understanding,
preferably but not necessarily quantitative.
The literature already has much to say about cracking of earth
dams. The emphasis, however, is on the mechanics of producing
the initial cracks, an aspect that has recently become at least
partly amenable to analysis. The analytical results serve auseful
purpose; reduction of cracking can undoubtedly be achieved
most successfully if the causes of cracking are understood and
avoided. Nevertheless, to accord with the principle of defence in
depth, every damshould be designed on the assumption that the
core maycrackand that thedamshould be safe even if it does.
So we reckon with the conclusion that modem dams seldom
if ever fail because of incorrect or inadequate numerical analy­
ses. They fail because inadequate judgement is brought to bear
on the problems that, whether anticipated or not, arise in such
places as the foundation or the interface between embankment
andfoundation. Sometimes they disclose themselves only in sub­
tle ways in theuse of the observational procedure. Irrespectiveof
specifications, contractual arrangements, possibilities of claims
for extras, or delays, these problems must be recognised and
solved satisfactorily.......
4 STATISTICS ON DAMINCIDENTS AND FAILURES
Some very informative descriptions and discussions of embank­
ment damfailures are presented by Sherard et al., (1963) and in
the books edited by Leonards (1985), Singh and Varshney
(1995), andJansen (1988) where lessons fromnotable events are
presented.
Table 2 shows examples of recent ICOLD conferences and
publications on the subject of safety, reliability andrisk.
ICOLD (1995) provides a world-wide review (except China)
including 52 concrete and 129 embankment dam failures and
their causes. This review shows clearly that failures, when they
occur, mainly take place very early in a dam’s life. Table 3
summarizes the specific information on the causes of failure for
the embankment dams considered in the study, includingfailures
during construction.
The information presented in Table 3 corresponds with the
results inTable 4 fromaprevious study of incidents and failures
registered for 240 embankment dams in the USA (USNRC,
1983). As can be seen fromboth tables, internal erosion consti­
tutes a prim
arycause of concernand will bediscussedin Section 5.
A closer study shows that the incidence of piping through the
embankment is about two times higher than piping through the
foundation.
Table 2. Recent ICOLD events focusing on dam safety
1993 “International Workshop on Dam Safety Evaluation",
Grindelwald, Switzerland.
1994 “Safety Assessment and Improvement of Dams", ICOLD
Congress, Question 68, Durban, South Africa.
1995 “Dam Failures - Statistical Analysis”, ICOLD Bulletin 99.
1996 “Current Issues and Advances in Dam Safety”. Interna­
tional Conference, Ontario, Canada.
1997 “Incidents and Failures of Dams”, ICOLD Congress, Ques­
tion 75, Florence, Italy.
1997 “Risk-Based Dam Safety Evaluation’’, International Work­
shop, Trondheim, Norway.
1998 “Managing the Risks of Project Development, Safety and
Operation”. International Conference, Buffalo, New York,
USA.
1998 “New Trends and Guidelines on Dam Safety", Interna­
tional Symposium, Barcelona, Spain.
2000 "The Use of Risk Analysis to Support Dam Safety Deci­
sions and Management", ICOLD Congress, Question 76,
___________ Beijing, China._________________________________________
2493
Table 3. Primary causes of embankment failures or partial failures (ac­
cording to ICOLD, 1995)
Causes of failure TE ER ER/TE
(%
) (%
) (%
)
Overtopping (of crown) 23 45 31
Internal erosion (piping) - in dam body 20 8 23
Internal erosion (piping) -in foundation 13 13 15
Other structural causes - e.g. slope instability and 29 25 23
settlements
Other causes 15 9 8
Total (percentage) 100 100 100
Total number of dams 92 24 13
TE= Earthfill; ER= Rockfill
Table 4. Causes of embankment incidents and failures according to US-
COLD (USNRC, 1983)
Causes of incident or failure % of 240 dams
External erosion (overtopping/wave action) 29
Internal erosion (in dam body/foundation) 38
Foundation instability 14
Excessive dam deformation 13
Deterioration (chemical/physical) 2
Malfunction of gate 2
Earthquake effects 1
Construction errors 1
The experience with the 175 large embankment dams in Nor­
way, the highest being 145 m, is described by Kjaemsli et al.
(1992) and Hfleg et al. (1993). Most of these are rockfill dams
with a broadly graded moraine core, but several of the recent
ones have asphalt concrete core (Hfieg, 1993; 1998). There has
been no failure of an embankment dam in Norway higher than
15 m, but of the 175 built, 32 have had some repair. Twenty
have sustained minor damage to their upstreamslope protection
as aresult of wave and ice action. Six have suffered some inter­
nal embankment erosion, in two cases probably preceded by hy­
draulic fracturing, and six have been affected by excessive or
differential settlement. A 10m high earthfill dambuilt in 1975
failed in 1976 as aresult of erosion along aconcrete culvert go­
ing through the moraine core - ingeneral, avery poordesign fea­
turewhich should be avoided.
Remedial work in Norway has consisted of improved rip-rap
design and construction, and internal erosion and leakage have
been controlled with water-cement-bentonite-sand mixture grout
injection. Of all the dams completed since 1976, only one has
required repair, demonstrating that lessons have been learnt from
the experience gained, and thatthere have been improvements in
design criteria andconstruction andcontrol procedures.
In summary, areview of the available statistics fromdifferent
parts of the world and accompanying evaluations and analyses
(for example Londe, 1993; ICOLD, 1995; ICOLD, 1997; Foster
et al., 2000a) show that the causes of damincidents and the fre­
quency of failure vary fromone region to another. However, the
average probability of failure per dam-year has been reduced
from around 10"
4 towards 10'5over the last 30 years. Further­
more, adambuilt some 30 years ago and still performing well is
as safe as a dam built with today’s state-of-the-art technology
andquality control.
In general, but excluding tailing dams, the safety record for
dams is good and it is steadily improving. However, there is no
room for complacency because we have had incidents and fail­
ures even with dams built during recent years (e.g. Teton Dam,
1976; Gouhou Dam, 1993), and continuous monitoring and
maintenanceof existing dams is mandatory (see Section 5).
As part of the US National Dam Safety Program, a National
Performance of Dams Programhas been established. The aimis
to ensure that safety related dam incidents and failures be re­
ported to a common information centre at Stanford University,
California. This will allow dam engineering and safety profes­
sionals to benefit from the lessons of in-service dam perform­
ance across the USA. It will further increase the probability of
including all potential incident and failure modes in future risk
analyses (see Section 6). Othercountries orregions should estab­
lish similar programs, because incidents do occur, but many are
not properly reported and analysed.
4.1 The cases of Gouhou Dam and Teton Dam
The failure during first reservoir filling of the 71 mhigh Gouhou
concrete face embankment dam, built in China in 1993, is de­
scribed by Chen (1993). Almost all modem concrete face em­
bankment dams are built of sound rock materials, while Gouhou
Dam consisted primarily of sandy gravel. When leakage devel­
oped through the concrete facing, pore pressures built up in the
sandy gravel in the downstream shoulder as the drainage provi­
sions were inadequate (see Section 5.4). The cross-section de­
sign and zoning did not adequately take into account the differ­
ences in material properties and behaviour between a good
rockfill, with gradually increasing rock size towards down­
stream, and the sandy gravel which was used. This led to the
complete damfailure when cracks developed in the concrete fac­
ing. Experience shows that opening ofjoints or cracks often oc­
curs in concrete facings and must be allowed for in the safe de­
sign ofthis type ofdam.
Teton Dam, Idaho, 93 m high, was built in a steep walled
canyon incised by the river into the Texburg Bench. The rocks
exposed in the canyon walls are almost entirely of volcanic ori­
gin. At the dam site, they consist primarily of intensely layered
andjointed rhyolite with minor inclusions of basalt, breccia, and
welded ash-flow tuff. The embankment was built mainly of the
locally available silt material.
Failure occurred during first filling of the reservoir in June
1976. Leps (1988) states that the lessons learned clearly do not
represent new lessons for the profession, but serve as essential
reminders of points sometimes ignored orforgotten.
a) The responsible design engineer should be required to visit
the construction site, perhaps monthly, to verify that site con­
ditions and construction materials conformto the design con­
cept and, if not, to determine required modifications.
b) The downstream contact of animpervious embankment zone,
whether against foundation materials or against amore pervi­
ous embankment zone, must be protected against piping by
use ofengineeredfilter zones.
c) Ingrossly pervious foundation bedrock, asingle grout curtain
should not be reliedupon to be adequately effective.
d) Whenever impervious borrow exists at moisture contents se­
verely below optimum, it should be mandatory initially to
moisture-condidon the material to near optimum, first in the
borrow area and thereafter, but to avery minordegree, on the
fill.
e) Deep, narrow, key trenches in bedrock, with steep side
slopes, should be avoided because they invite arching of
backfill as it settles, and thereby establish unfavourable stress
conditions that are conducive to hydraulic fracturing.
f) Because of inevitable hydrologic uncertainties, and difficul­
ties in forecasting precisely when critical water control out­
lets may be completed and serviceable, it is frequently almost
academic to assume that it will be possible to control the rate
of initial reservoir filling. Hence, the dam designer should
fully consider that the reservoir may fill very quickly, regard­
less of the generally assumed merit of controlling the filling
rate.
g) It is unlikely that, even if extensive instrumentation had been
provided, any useful timely warning of impending failure
would have been sensed and evaluated in advance of the sud­
den, veryrapidfailure ofTeton Dam.
4.2 The case ofmine tailing dams
Mine tailing dams are not included in the surveys and statistics
referred to above. They show a relatively poor safety record,
which must be improved by getting more dam engineering
2494
know-how into the design and construction of these types of
structures built by the mining industry (ASDSO 2000b).
Morgenstem (1998, 2000) refer to eleven serious incidents over
the short period 1995-1998 associated with mine tailings and
waste overburden management, and several incidents and fail­
ures have occurred since that time. Morgenstem states that all
were modem structures and “were not part of the historical leg­
acy of poorly engineered waste containment structures that char­
acterized parts of the miningindustry in the past”.
Clearly the state of the art and practice for these types of pro­
jects is not satisfactory, and recent efforts by ICOLD, the UNDP
and the mining industry have increased the awareness of this
situation.
5 PERFORMANCEEVALUATION, SAFETY ASSESS­
MENT AND REMEDIATION
The ageing dampopulation requires regular maintenance andre­
habilitation (e.g. Penman and Milligan, 1993). In addition,
strengthening may be required to satisfy current safety and risk
criteria based on state-of-the-art knowledge. Society will have to
spend significant resources in the years to come to ensure thede­
sired performance and safety of our dams. In recent surveys by
ASCE (1998) and ASDSO (2000a) the latter estimates that
US$ 40 billion is needed to properly rehabilitate and upgrade
dams in the USA.
In general, embankment dams have shown to be very resis­
tant to earthquake shaking. However, due to the potential lique­
faction hazard for old hydraulic fill dams and dams resting on
loose alluvial foundations, strengthening has been found advis­
able in a number of cases (e.g. Seed, 1979; Marcuson et al.,
1994; Finn, 1996). The case study presented by Gillon et al.
(1998) for the extensive upgrading of Matahina Dam, New Zea­
land, is most informative. However, this topic will not be further
addressed herein.
Quite often the reasons for excessive leakage, internal ero­
sion, excessive displacements, differential settlements or crack­
ing in an embankment dam may not be obvious. Careful inter­
pretation of observations, visual and through field instruments,
must be carried out to assess the situation before specific meth­
ods of repair or upgrading are decided upon. Unexpected obser­
vations may not give any reason forconcern if alogical explana­
tion can be found. Three questions should be answered during
the evaluation:
• What is “abnormal” embankment behaviour?
• Does the deviation from predicted behaviour indicate lower
safety than aimed forin the design?
1 = moraine core;
2 = sandy gravelfilter;
3 - transition rockfill;
4 = supporting rockfill;
5 - slope protection
6 =protective cap ofselected
blocks: and
7 = grout curtain
• Does thedeviation require remedial action?
In the following sub-sections, four aspects of embankment
dam behaviour are considered. They illustrate the need for cor­
rect interpretation of observations before the diagnosis is given
anddecisions are made how to remediate.
5.1 High pore pressures in the earth core
In several embankment dams with earth core, the measured pore
pressures in the downstream portion of the core have been re­
portedto be much higher than predicted duringdesign. Two well
documented studies are the Svartevann Dam, Norway (Kjaemsli
et al. 1982; DiBiagio et al., 1982) and the WAC Bennett Dam,
British Columbia (Stewart and Imrie, 1993). Did the high pore
pressures indicate that critical cracks or “channels” had devel­
oped through the core?
Figure 1shows the maximumcross section of the 129 mhigh
Svartevann rockfill dam with a slender and inclined broadly
graded moraine core, founded on bedrock. Figure 2 shows the
measured piezometric heads versus reservoir level in three pie­
zometers at el. 810 located in the core upstream, in the centre
and downstream, respectively. In total 24 electric closed-system
piezometers (vibrating wire) were located in this same core
cross-section. Piezometer P12 gave readings that consistently
fall on the 45° line in Fig. 2, showing that the measured pore
pressure close to the upstream face of the core was equal to the
water pressure in the reservoir at that level. During the first year,
piezometer P14 showed much higher pore pressures than those
predicted based on conventional theory of saturated steady-state
flow. However, after two full cycles of seasonal lowering and
raising of the reservoir, the piezometric head in P14 had de­
creased significantly, approaching the theoretical solution. Fig­
ure 3 shows the piezometric head versus time for PI2, PI3 and
P14 up until 1989, 13 years after end of construction. The reser­
voir level at any given time is that recorded by piezometer PI2.
Equilibrium has been reached, and there is no further reduction
in the pore pressures on the downstream side, as P14 only re­
flects the changes in reservoirlevel.
S i i4»i i '« J i ' 1 f •1.774.5
JUjlg M 1^ w rw ^T U 'ja J W ffT T O
0 100 m
The Svartevann rockfill dam during construction.
Vatnedalen Damin Norway (125 m) shows similar trends forthe
measuredpore pressures (Myrvoll et al, 1985), as well as several
other dams described in the international literature. Many hy­
potheses have been proposed over the years, and the following
are some of the explanations presented for the unexpected pore
pressures:
Figure 1. Cross-section and photo of the Svartevann Dam, Norway.
2495
R
*s»rvouw
atmta
v
eltm
l
Figure 2. Measured piezometric heads versus reservoir level from
1975-1979 for Svartevann Dam.
(i) Heterogeneities, construction imperfections and larger hori­
zontal than vertical permeability are not properly considered
in the prediction analyses. Therefore, the downstream pore
pressures are underestimated.
(ii) Excess construction pore pressures remain in the core for a
longer time thanpredicted.
(iii)A lower permeability coefficient on the downstream side as
aresult of higher effective stresses thanon the upstreamside
(deMello, 1980; Vaughan, 1989).
(iv)Cracks initiated by hydraulic fracturing caused by arching
effects and locally lowered effective stresses in the core (for
example Sherard, 1984; 1986; de Fries, 1991). Pore pressure
communication through the cracks gives high pore pressures
downstream.
(v) Migration of fines from the core to the downstream filter,
which becomes “clogged”. There will then be overpressures
in the downstreamportion compared with those predicted in
a conventional analysis (Peck, 1990; Stewart and Imrie,
1993).
A satisfactory hypothesis or combination of hypotheses must
not only be able to explain the high temporary pore pressures
downstream, but also the decrease that has been measured with
time. Since the presentation of the “abnormal” pore pressure ob­
servations fromthe Svartevann and WAC Bennett dams, Hydro-
Québec (Canada) has reported several similar cases. First St-
Amaud (1995) and then Dascal (1995) offer the following ex­
planation:
(vi)After compaction, the material in an earth core is usually not
saturated (typically 50-90 percent).
—During reservoir impoundment, air (gas) is trapped in the
submerged zones. The pressure measured by closed-
system piezometers in partly saturated soils is the air pore
pressure, which, in general, is higher than the pore water
pressure.
—The permeability coefficient upstream increases as the air
bubbles are dissolved or transported down stream.
—The pore pressures decrease, and therefore the volume of
free gases increases in the direction of flow. Furthermore,
dissolved gases in the waterupstreamcome out of solution
towards downstream. Thus, the degree of saturation and
core permeability decrease towards downstream.
—This contrast in permeability, which can be quite sig­
nificant, causes pore pressures downstream which are
much higher than those predicted from a seepage analysis
for ahomogeneous core.
—Some blockage of the flow will exist as long as free gases
are present. Reaching full saturation and steady state flow
may take a long time. Until then, there will be pore over­
pressures in the downstreamportion of the core.
There will not be one hypothesis which satisfactorily explains
all cases and situations encountered or reported in the literature.
However, explanation (vi) seems well founded, and may apply to
many dams, e.g. Svartevann, where cracking, erosion and trans­
portation of fines are not the reasons for the unexpected pore
pressurebehaviour. At Svartevannthe decrease in measured pore
pressures started after only a short time, while at WAC Bennett
it took several years before the trend turned (Stewart and Imrie,
1993). Further theoretical and experimental studies sponsoredby
Hydro-Québec andothers have recentlybeenundertaken to more
fully understand and test the hypothesis presented by St-Amaud
(1995), and they support the concept (CGS, 2000). High down­
stream pore pressures due to this phenomenon will not require
remedial work, while internal cracking and crack erosion may
call forrehabilitation by grouting orother measures.
5.2 Large post-construction displacements
Pore pressures and displacements measured during embankment
construction give information about the deformation properties
of the foundation and of the materials compacted in the different
embankment zones. The measurements are of value when pre­
dicting displacements caused by further embankment construc­
tion and reservoir filling, and post-construction movements with
time. Post-construction displacements of large dams are usually
900
880
860
340
/ Y
U
■ ( v
4
y
V V / s /
4
I j
*
9
P12
y
V
V * r
V
N s ' s
y  y
v
V
A P13
/
[ /
ÿ 
v V
V V
V V V /-
v y V
i i
j
V
—
•*— * v __ — - P14
rfSB
S?
820
800
780
1974 1875 1978 1977 1878 1379 1880 1381 1982 1983 1984 1985 1988 1987 1988 Ì989
E
n
do!contract»» T
imtly.*(|
Figure 3. Measured piezometric heads versus time from 1973 to 1989 for Svartevann Dam
2496
measured, at least at the crest, while measurements in the interior
are more rare. The magnitude and rate of post-construction dis­
placements are often taken as anindication of the “health”of the
embankment by comparing with corresponding measurements
fromotherstructures reported in the literature.
When this is done, and to evaluate whether the displacements
are abnormal or not, it is important to specify the location of
each measurement point and the time of the first measurement
after end of construction (that is, the reference value for subse­
quent measurements). It is not uncommon for the vertical dis­
placement component of the upstream crest bolt to be signifi­
cantly larger than the settlement of the corresponding
downstream crest bolt. This is primarily caused by the raising of
the reservoir, especially the last 30 per cent up to the maximum
level, unless the reservoirhas been filled simultaneously with the
embankment construction.
Inseveral cases, the increased compressibility andsubsidence
of the upstream shoulder on submergence has caused a relative
slip between the fill and the core in the upper part of the em­
bankment. This results in differential settlements across the crest
and possibly longitudinal cracks along it. The phenomenon is of
no real concern with respect to dam safety, as the movements
stabilize after the first reservoir filling, lowering andrefillingcy­
cle, and cause no transverse cracks. The observation does not
call for a flattening of the upstreamslope, but possibly some re­
pair to the rip-rap protection (e.g. Paré, 1984; Hóeg et al, 1996).
Table 5 gives the measured post-construction crest settle­
ments (upstream, top of thecore anddownstream) forsome large
Norwegian rockfill dams built since 1972 on stiff foundations.
The dams above the double horizontal line in Table 5 have cen­
tral or gently sloping clay moraine core, while the dams below
have thin asphalt concrete core. It can be seen that the Vatneda-
len I and Deg dams have very small core- and downstream set­
tlements, but fairly large upstream settlements. This is because
of the rockfill saturation effect described above, resulting in lo­
cal subsidence in the top part of the upstream slope. The up­
stream slope for the Vatnedalen dams is 1V:1.5H and for Deg
dam 1V:1.6H.
Table S. Post-construction settlements for Norwegian rockfill dams on
stiff foundations
Dam Year H
(m)
Vertical settlements (%H)
Crown Top Crown
upstream core down­
stream
Oddatj0m 1987 145 0.26 0.20 0.22
Svartevann 1976 129 0.80 0.80 0.65
Vatnedalen I 1983 125 0.90 0.20 0.27
Deg I 1972 90 0.70 0.15 0.15
Nyhelleren 1979 85 0.12 0.12 0.12
Vatnedalen II 1983 60 0.10 0.10 0.10
Juklal 1973 59 0.60 0.65 0.33
Storvatn 1987 90 - 0.20 -
Berdalsvatn 1988 65 018 0.14 0.10
Styggevatn 1989 52 0.12 0.20 0.10
Riskallvatn 1986 45 0.20 0.15 0.10
Storglomvatn 1997 125 0.20 0.16 0.11
Figure 4 gives a simplified overview of the measured post­
construction crest settlements for rockfill dams worldwide, built
on stiff foundations. The data have been collected from several
authors (Soydemir and Kjaemsli, 1979; Clements, 1984; Dascal,
1987; andHOeget al., 1996), and the scatteris significant. Inthe
literature it is not always indicated where across thecrest the set­
tlements are measured (upstream or downstream). Most rockfill
dams built of sound rock since 1970 show a trend that gives a
post-construction crest settlement in the range of 0.2-0.4% of
the maximumdam height after 25 years of operation. The trend
is approximately linear with the logarithm of time, and there is
no clear indication that high dams give a higher normalized set­
tlement than lower dams. Some modem dams are reported to
have settlements considerably larger than those indicated above.
but no satisfactory explanations have been presented.
For older dams, built mostly without rockfill compaction, the
normalized post-construction settlements are considerably larger
and the scatterin the results much greater (Fig. 4).
Post-construction displacements of dams on stiff foundations
dependon many factors, including;
— properties of rockfill andcore materials;
— layer (lift) thickness andcompaction effort;
— sluicingof rockfill during placement;
— steepness of exterior slopes;
— shape of valley;
—upstreamimpervious face orcentral core;
— zoning ofembankment;
— otheraspects.
However, some important factors are sometimes overlooked
when displacements are evaluated and compared with corre­
sponding measurements from other embankment dams. These
are:
— the location of points on the crest where measurements are
taken;
— time of first crest measurements after the completion of con­
struction (a significant part of the long-term settlement takes
place during the first few months);
— reservoir level at the end of construction when crest settle­
ment bolts were installed;
— rates of damconstruction andreservoir filling;
— magnitude of reservoirfluctuations.
These aspects make it difficult to make “fair” comparisons
such as those proposed in Table 5 and Fig. 4, but the factors
must be considered before onejudges whether the recordedpost-
constructiondisplacements are “abnormal” or not. If, in addition,
the damsits on an inhomogeneous and compressible foundation,
the comparisons are that muchharderto make.
5.3 Internal erosion - will dam selfheal?
As presented in Section 4, many incidents andfailures havebeen
attributed to internal erosion. Our concern has grown in recent
years as it has been clearly documented that damaging internal
Figure 4. Measured post-construction crest settlements for rockfill dams
built on stiff foundations
erosion may not only show up during initial filling of reservoir
or shortly thereafter, but first several years later (Marsal and
Pohlenz, 1972). As safety evaluation of ageing dams is receiving
increased attention, so is the topic of possible internal erosion
developing at a later stage in adam’
s life. Charles (1997) gives
an excellent overview, and recent papers are for instance pre­
sented by Fosteret al. (2000b).
2497
In many instances of increased leakage of turbid(muddy) wa­
ter, clearly indicating a process of ongoing internal erosion, the
leakage has stopped almost as quickly as it started, returningto a
normal seepage rate. Erosion “pipes” which had started to de­
velop, collapsed and closed, as the downstream filters had been
working after some transport of fines from the core had taken
place. It points to the essential role of proper filter design crite­
ria, which have become much stricter in recent years. Starting
with the classical work by Terzaghi in the 1920s, very many en­
gineers have studied filter requirements and properties. The cri­
teria by Kenney and Lau (1985) and Sherard and Dunnigan
(1989), and summarized by ICOLD (1994), represent the state of
the art. There are specialty conferences regularly organized on
this topic alone (Wolski and Mlynarek, 2000), and Vaughan
(2000) presents recent reviews and evaluations. However, good
filter design criteria by themselves are not sufficient to ensure
satisfactory performance. The field placing process and control
is just as important to avoid segregation and inhomogeneous fil­
ter properties leading to local weak spots which the seeping wa­
ter is sure to find. This is one of the ’’extreme value problems”;
as defined by de Mello (1977), andit calls for “defence indepth”
(Section 3).
5.3.1 Initiation ofinternal erosion
Inadequate filters do not cause erosion, which is initiated by one
of the mechanisms described below, but they fail to halt (arrest)
erosion which has started and which may lead to damage oreven
damfailure.
Flowing water exerts drag forces on the soil particles in the
direction of flow, and these drag forces increase with flow veloc­
ity. Intergranular contact stresses, interlocking and any true co­
hesion (cementation) between particles prevent themfrombeing
tom loose, unless a critical flow velocity is exceeded. This criti­
cal velocity therefore depends on material properties and the lo­
cal effective stress condition.
The phenomenon of mechanical internal erosion may be clas­
sified into four main categories: piping, internal mass erosion
(suffusion), contact erosion andcrackerosion. However, the ero­
sion process may well start by one mechanismandgradually de­
velop into another form, e.g. start as mass or crack erosion and
develop into piping. Piping is the most dangerous of the mecha­
nisms, because due to the process of backward erosion, the se­
verity of it may not be detected until the pipe (eroded canal)
breaks through on the upstream side in direct contact with the
reservoir. The internal erosion may also cause sinkholes on the
crest or upstream slope of the dam, which in turn may lead to
overtopping.
The case studies reported in the literature often refer to in­
adequate filters as the cause of the incident or failure and there­
fore fail to identify the real cause oferosion initiation which may
have been one ofthe following:
• Unfavourable properties of core material which was easily
erodible (i.e. internallyunstable), dispersive, or in some cases
partlydissolved due to chemical reactions;
• Inadequate core material compaction, e.g. due to unsatis­
factory quality control;
• Vertical and narrow core between stiff adjacent zones which
led to arching action, reduced effective stresses, hydraulic
fracturingandcrackopening;
• Inadequate preparation and sealing of fractured rock foun­
dation or abutment, which also may have had crack infill or
wall material subject to dissolution;
• Narrowcut-offtrench underthecore in inadequatelyprepared
fractured rock. A trench which is too narrow may lead to
arching, reduced effective stresses and erosion or hydraulic
fracturing;
• Embankment design not adapted to a foundation overburden
with greatly varying compressibility or depths to bedrock
across the valley floor. This caused differential settlements
and transverse cracking or zones with very low effective
stresses;
• Inadequate compaction and low contact stresses against cul­
vert, sheet pile wall or concrete structure leading to contact
erosion;
• Design and construction not adapted to unfavourable topo­
graphy with local depressions and protrusions in foundation
and abutments. This may lead to low local effective stresses
and cracking. In a narrow valley one may also get significant
arching between the abutments and reduced effective stresses
in the lower portion of core;
• Reduction in local effective stresses and cracking due to dif­
ferential displacements caused by uneven regional subsidence
or fault movements;
• Theory and practice indicate that the probability of crack-
opening in the core increases with increasing rate of em­
bankment construction andreservoirfilling rate. There is then
too little time allowed for the different embankment zones to
adjust among themselves to the changing loading conditions.
Recent experience has shown that earth core material around
and in the vicinity of vertical instrument cables and pipes (in­
strument islands) is not (cannot) be compacted properly. This
has, for instance, led to local settlements (collapse) upon wet­
ting, sinkholes, local internal erosion, internal loose zones or
even cavities. This method of instrumentation must be re­
considered. Furthermore, the local observations and occurrences
at such instrument islands may not give reliable indications of
the well-being of the embankment in general, and incorrect con­
clusions may be drawn about thedamperformance.
If properly placed, filters may prevent transportation of parti­
cles out of the core and thus arrest the erosion process that has
been initiated by one of the mechanisms listed above. The design
of the damand the filter zones must be such that settlements and
distortions do not impair or weaken the functioning of the filters.
Few, if any, of the 122 Norwegian large rockfill embankment
dams with broadly graded moraine core satisfy today's strict fil­
ter criteria, which in most cases will require mechanical process­
ing of the filter material. The reason for not having experienced
more than a few incidents of damaging internal erosion is that
the critical flow velocity has not been exceeded, or that the fil­
ters locally have been adequate although they were not designed
to satisfypresent state-of-the-art criteria.
In addition to the mechanical erosion phenomenon described
above, one may face the problem of dissolution (chemical ero­
sion) of the material. Incore construction one must avoid the use
of materials that will be dissolved by the seeping water. One
must then also consider possible changes in reservoir water
chemistry with time for instance due to pollution. The presence
of dissolvable materials in the damfoundation (e.g. karst) repre­
sents a more challenging task for the designer, as discussed by
Jansen (1988). That may require the use of extensive and multi­
ple-rowgrout curtains orpositive cut-off walls.
5.3.2 Examples ofrecent dam cross-sections
The concern about the potential hazard of internal erosion in
earth cores has in some cases been the argument for choosing a
design with upstreamconcrete facing or interior asphalt core, al­
though earth core material was locally available. In other cases,
of course, climatic conditions and construction scheduling and
duration, have been the factors which decided against the use of
acompacted earthcore.
The West Dam of the Eastside Reservoir in Southern Cali­
fornia is an example of a recent rockfill structure with an earth
core built to high quality and state-of-the-art standards wrt. in­
ternal erosion resistance, filter design and construction (Forrest
et al., 1997; ENR, 1997). Among several alternatives considered,
an earth core design was selected. The earth core has a maxi­
mumheight of 102 mandthe damlength is 2,500 m. It is anoff-
river reservoir built to provide emergency water supply in a
strongly seismic region. Therefore, it is a conservative design
with a wide core, generous fillers of processed materials and
gentle exterior dam slopes. A 40 m deep cut-off wall of plastic
concrete through the alluvium and keyed into bedrock virtually
2498
eliminates foundation seepage and any possibility of internal
erosion in the highly variable andinhomogeneous foundation.
Figure 5 shows the cross-section design forthe modemOdda-
tjttm rockfill dam (145 m high) with an earth core of broadly
graded moraine (Kjimsli et al., 1992; Windisch and HOeg,
2000). The damwas completed in 1986 and is based on previous
experience with many similar but lower dams in Norway. The
photo shows the dam located in the Norwegian mountains to­
gether with two other dams to create the reservoir for hydro­
power.
Figure 6 presents the cross-section design for a modem con­
crete face rockfill dam (CFRD), and the photo shows Foz do
Areia Dam in Brazil, 160 m high, completed in 1980 (Cooke,
1998; 1999).
Figure 7 presents the cross-section design for a modem as­
phalt concrete core rockfill dam (ACDR) (Hoeg, 1993) and a
photo of the recently completed Storglomvatn Dam, Norway. So
far this is the highest damof its kind (125 m), but several higher
ones areunderconsideration.
5.4 Drainage capacity and resistance to leakage or over­
topping
In the design of new embankment dams as well as in the safety
evaluation of existing ones, one must assume that temporary sig-
Figure 5. Cross-section of OddatjOm rockfill dam (145 m high) with inclined moraine core. Photo shows OddatjCm Dam on the left (Fjellanger
Wider0e A.S.)
Fac*slao
1A = Impervious soil; IB = Random fill, 0.5 m layers; 2A = Processed
fine filter; 2B = Crusher-run rockfill; 3A = Selected small rock placed in
same layer thickness as Zone 2; 3B = Quarry-run rockfill, about lm lay­
ers; 3C = Quarry-run rockfill, about 2 m layers; 3D = Dumped rockfill
(optional). Compaction for rock zones; four passes of 1 0 1 vibratory
Figure 6. Cross-section of a modem CFRD of sound rockfill on a sound rock foundation (Cooke, 1998). Photo shows Foz do Areia in Brazil, 160 m
high (Cooke, 1999).
1 = asphaltic concrete core; 2 = gravel transition, 0-60 mm;
3 = crushed rock transition, 0-200 mm; 4a = rockfill, 0-400 mm
4b = rockfill, 0-800 mm; 5 = rip-rap; 6 = crown cap, large blocks
7 = toe drain, large blocks > 0.5 m3
Figure 7. Cross-section of Storglomvatn rockfill damwith vertical
as it was being topped offin 1997.
asphalt concrete core (ACRD). Photo shows the dam(125 mhigh)
2499
nificant interior leakage may occur. The dam must be able to
safely accommodate such a leakage until it either selfheals, the
reservoir level is lowered, or remedial work is done. This re­
quires that the downstreamdrainage capacity is designed to han­
dle the leakage without the occurrence of scour and unravelling
or local slope instability thatbyprogressive action mayendanger
the safety of the structure. Satisfactory drainage capacity pro­
vides the second line ofdefence (de Mello, 1977; Peck, 1980). In
general, rockfill dams have inherently much higher resistance
than earthfill dams as they tolerate orders of magnitude larger
leakage rates before afailure situation develops.
A comprehensive andconcise definition of the termrockfill is
difficult and varies from one country/region to another. Leps
(1988) proposes that to be termed rockfill, the material must
have an average particle size of at least 50 mm, and no more
than 40%of the average sample should be smaller than 25 mm.
Thus, a limit is imposed on the finer fraction, but no limit is im­
posed on the maximum particle size. If the percentage of minus
25 mm material exceeds 50%, that fraction will begin to domi­
nate the stress-strain and permeability properties, as it becomes
the matrix that, when perfectly blended, completely surrounds
and separates the larger rock particles. The result is lower shear
strength and lower permeability, andthereby adiminution of the
fundamental assets of rockfill.
The particle size referred to is that after compaction, which
may be significantly smaller than that taken out of the quarry,
borrow area or tunnel excavation. The extent of crushing de­
pends on rock type, mineralogy and compaction equipment and
procedure. The average gradation of a lift may be a misleading
characteristic in that the fill is never perfectly blended. The
coarser particles always concentrate at the bottom of each lift
andthe finer constituents at the top.
5.4.1 Failure mechanisms
In the safety evaluation of existing structures, one often finds
that present hydrological information and design criteria lead to
higher probable flood levels than the dam originally was de­
signed for. This may be due to changes in climate andincrease in
precipitation levels. Therefore, the resistance of the damto over­
topping must be assessed. The remedial work may consist of
dam heightening, armouring the dam crest by roller compacted
concrete (RCQ, andreinforcing the downstreamslope.
In a systematic risk analysis (see Section 6), not only the fail­
ure probability, but also the probable consequences of down­
streamdamage in case dambreach should occur, must be evalu­
ated. The extent of damage, particularly the potential loss of
lives, depends entirely on the warning time available for the
evacuation process. The warning time depends on the speed with
which the failure (breaching) process andflood wave develop.
Failure of a typical rockfill dam with anearth or asphalt core
or an upstream facing, may be precipitated by one of several
mechanisms, including:
• Scour andunravelling of the downstreamtoe;
• Scour andunravelling of the downstreamslope above the toe;
• If the mechanisms above are prevented, failure by a more
deep-seated sliding surface due to build-up of pore water
pressures in the downstreamfill.
If the rise of the reservoir is so rapid that not only the core is
overtopped, but even the dam crest, other failure mechanisms
may also develop (e.g. Leps, 1972; Parkin, 1991; Toledo, 1998).
The overtopping may be caused by obstructed discharge facili­
ties during a flood or by sinkholes caused by severe piping due
to internal leakage anderosion.
Much research effort is now going into better defining the re­
quired drainage capacity, the resistance to overtopping, the
breaching process andthe characteristics of the flood wave in the
unlikely event that disaster strikes. Laboratory modelling tests,
field tests and numerical simulations have been used in this ef­
fort (e.g. Fread, 1987; Yang, 1997; ICOLD, 1998). In Norway,
for instance, a program is now underway (2001-2003) to study
the behaviour of typical rockfill embankment dams under such
extreme flow conditions. The program will include 6 m high
field “model” embankments built specifically for this purpose,
and brought to failure. The model dams are located immediately
downstreamof anexisting dam, so the inflow may be accurately
controlled by the gates.
Rockfill dams built in Norway since 1980 have all been de­
signed with a special toe drain consisting of rocks larger than
0.5 m3 (see Fig. 5). When evaluating the drainage capacity of
older dams, one must judge whether the rock size in the toe is
sufficient to resist the rate of flow caused by a leakage incident
of a specified low probability. The smallest stones in the toe will
become unstable and unravel early in the process, but that may
not have any effect on the overall stability of the load carrying
skeleton of the toe. Reliable criteria do not exist for what grain
size diameter to consider, e.g. d20 or dj0, and the effect of the
shape of the grain size curve (i.e. uniformity coefficient). The
planned research will address this and other issues, in order to
derive criteria for strengthening existing toes and downstream
slopes to resist accidental leakage andtemporary overtopping.
6 SYSTEMATIC RISKANALYSIS
A useful definition of risk is the computed product of the prob­
ability of failure (or damage) and the expected cost (direct and
indirect) of failure or damage, should it occur. However, fre­
quently in the literature and in the media one will also find that
the wordrisk refers to probability of failure alone.
When evaluating expected costs and consequences, one con­
siders potential downstreamdamage in terms of loss of life, inju­
ries, environmental and social effects, and material losses. There
are special considerations for a cascade development along a
river, andthe role of warning time achieved through surveillance
and monitoring. The time delay in the dam-breach and flooding
process may be crucial for the extent of the consequences, and
appropriate preparedness and action plans may substantially de­
crease the computed risk (Lafitte, 1997; Funnemarket al„ 1998).
The first papers on the potential usefulness of risk analysis in
dam engineering appeared 25 years ago, and in other fields the
methodology is being applied fairly extensively. There is now a
renewed interest in probabilistic risk analysis for dams, and
ICOLD is in the process of preparing “Guidelines on Risk As­
sessment for Dams". Kreuzer (2000) and Stewart (2000) recently
presentedcomprehensive overviews.
The main purpose of carrying out arisk analysis is to provide
decision support. For many applications, the resulting numerical
values do not have to be accurate in absolute terms, but must be
inherently consistent so they allow reliable relative comparisons
among alternatives. Going through such a systematic procedure
gives insight which is an essential outcome in itself, and has di­
dactic value for owner, operator, consultant and safety profes­
sional. The procedure pinpoints specific features and conditions
of the damandits operation where the largest riskreductions can
be achieved.
Risk analysis provides a framework for systematic appli­
cation of engineering judgement and available statistics in deci­
sion making. In this process it is common to use logic trees like
event and/or fault trees. An event tree is constructed for each
possible failure or damage mechanism. It is essential to decom­
pose each potential failure sequence into its components, thus
defining branch points in the event tree. The better defined the
mechanism and failure sequence, the easier it is to assign event
probabilities, and the more reliable the failure probability esti­
mate.
The probability estimates at each branch point in the tree may
be determined fromacombination of:
2500
• Statistical information relevant to the situation;
• Probabilistic estimates obtained by introducing parameterun­
certainties in the deterministic model for the event consid­
ered, including information qn the dam’
s performance so far;
and
• Engineeringjudgement quantified by subjective probabilities.
• The riskanalysis methodology maybe used:
• At the dam design stage to ensure that the main efforts are
placed where the uncertainties and theconsequences of unsat­
isfactory behaviour are the largest;
• When re-evaluating safety of anexisting dam;
• When selecting among different remedial actions for a par­
ticular dam and among dams in a cascade development (pri­
oritising);
• When establishingemergency action plans andpreparedness;
• To relate damengineering risk levels to acceptable (tolerable)
risklevels established by society.
The first four applications have proved to be very useful and
are not controversial. The fifth application is very complex and
the issue is sensitive as “acceptable risk” is not well defined.
There will always have to be a trade-off between extra safety
(reduced risk) and the increased use of society's resources. Inthe
old days, engineers managed to agree on and get acceptance for
using numerical values for safety factors. The public did not
really know what they implied, but the factors gave a feeling of
safety. We can no longer hide behind such deterministic factors
without defining what they imply. Probabilistic risk analysis can
assist us. However, to be accepted, the riskanalyses must be pre­
sented as credible, defensible, and transparent (e.g. Hartford,
1997).
A reservation (or criticism) against probabilistic risk analysis
is that one may overlook a future incident which would involve
one or more failure mechanisms not included in the analysis.
That is a most important concern and was referred to in Section
4. However, that concern is the same forour deterministic analy­
ses. Statistics show that it is the overlooking of aspects, not in­
adequate details of analyses, which cause unsatisfactory per­
formance andsometimes failure.
The first step in aprobabilistic risk analysis is to carefully go
through a "failure mode screening" where one visualises andde­
fines all potential failure modes. No probabilities are assigned at
this stage, but some failure modes are eliminated by physical
reasoning, and the arguments for elimination are recorded. Then
anevent tree maybe constructed where the failure sequences are
developed and detailed, displaying the interrelationships among
events. The process may stop at this stage without providing
quantitative probability estimates at each branch point in the
event tree. A very systematic way of performing a failure mode
screening is by means of the so-called failure modes and effects
analysis (FMEA). This may be extended to a failure modes, ef­
fects and criticality analysis (FMECA) as described in BSI
(1991) and applied by Beak et al„ (1997), Sandilands et al.
(1998), andMcLeod andPlewes (1999).
After several years of optimismin the profession with regard
to developing and performing meaningful quantitative probabil­
istic risk analyses for dams and auxiliary structures, there now
seems to be atrendtowards more use of the qualitative FMECA.
However, with time there will be increasing pressure from the
decision makers to quantify the risk level estimates so they may
be compared with an "acceptable risk" or "public protection
guidelines". In the Netherlands the development in this direction
is quite advanced and used in the safety evaluation and upgrad­
ing of dikes and stormsurge barriers (Vrijling, 2001).
7 NEED FORDAMSAFETY LEGISLATIONAND DAM
ENGINEERINGEDUCATION
The approaches used to ensure dam safety in different regions
and countries vary. For example, in Europe, more so than in
North America, one is inclined to use safety legislation, codes
and guidelines. Some of the reasons for the emphasis on this
topic are (Hfleg, 1998):
• Society today, more than arelatively few years ago, demands
that safety evaluations be carried out and documented for ac­
tivities involving risks imposed on the public (as opposed to
voluntary risks). Similar demands apply to certification and
re-certification of nuclear power plants, chemical plants, off­
shore structures, bridges andinfrastructure in general.
• More extensive records, and possibly changes in climatic
conditions since the construction of a dam, necessitate updat­
ing of flood estimates and re-evaluation of dam safety. For
instance, the flooding and dramatic failures in Saguenay in
July 1996 have had important impacts on legislation and
guidelines in Quebec, Canada.
• Earthquake effects may have to be considered in regions ear­
lierclassified as non-seismic.
• Significant changes in physical conditions both upstreamand
downstream since the dam was built require a review of the
risks involved andthe damsafety.
• There are significant differences among damowners and op­
erators with respect to their qualifications and the rigour of
their safety programmes, which must be updated to reflect:
new information obtained from available data and statistics;
improved understanding of failure and damage mechanisms;
changes in general international safety standards; and the
need for more objective approaches than were practised ear­
lier.
• The recent deregulation of the energy market in many coun­
tries has resulted in changes in dam ownership, and placed
more emphasis on required return on investment. One may
therefore fear that alower priority may be placed on safety.
• Environmental, social and dam safety considerations are
closely interrelated. Hence, safety is brought into focus in the
public debate, and more documentation is required relating to
reliability and risklevels.
• As stated in Section 5, ageing dams require continuous main­
tenance and rehabilitation, and strengthening may also be re­
quired. At the same time, and in many countries, the new
generation of engineers responsible for this work receives
very little hands-on experience with the design and construc­
tion of new dams, and relevant educational programmes in
universities are gradually disappearing. Therefore, the use of
dam safety legislation and fairly detailed requirements and
guidelines are considered to be awayof ensuring safety.
Regarding this last point it is interesting to note what Ter-
zaghi said about education and practical experience in his Presi­
dential Address at the 4. ICSMFE (1957):
“After the student has absorbed the theory of structures, soil
mechanics andengineering geology with his head andhas passed
the final examinations, his real development starts. The final
outcome depends entirely on innate qualifications and environ­
ment. Many of those who have passed their examinations with
flying colours are doomed to remain technicians to the end of
their lives. They will never leam to walk without the crutches of
step-for-step logical reasoning and no systemof education could
change this condition. However, the same individual may turn
into apoor technician or afirst-class one depending on the qual­
ity of the professional training he received, and that is important.
Those few who were bomunder a luckier star mayrise gradually
from the ranks of technicians to those of competent engineers,
capable of thinking with both their heads andtheirhips.
However, for given innate qualifications, the person with su­
perior training has atremendous advantage over the one who has
received adeficient education. Therefore, engineering education
should always be forus a matterof primaryconcern. Yet no mat­
terhow adequate the training may be, the prospects ofthe gradu­
ate to rise above the level of a technician are nil, irrespective of
his innate qualifications, unless the following additional condi­
tion is satisfied. His subsequent professional activities must give
him ample opportunity to compare his design assumptions and
forecasts with the real conditions as disclosed by the subsequent
2501
construction operations and the performance of the completed
structures. Otherwise he lives, without knowing it, in afictitious
world."
Terzaghi searched for "men of judgement", to use his own
phrase. In many parts of the world, e.g. Europe andNorth Amer­
ica, such damengineers will be hardto find, unless they get their
experience fromcountries where dams are being built, or special
field training programs are established. This is a challenge - the
recruitment, education andpractical training of damengineers to
take care of and upgrade where required, the aging dampopula­
tion.
7.1 Application o fnew criteria to old dams
There is controversy about how new safety criteria shall be ap­
plied to existing structures, built under the regime of different
criteria. In any such re-evaluation of an existing dam, due con­
sideration must be given to the dam's performance duringopera­
tion to date. With time, some of the uncertainties which had to
be accounted for in the initial design and therefore may have re­
quired a higher design factor of safety (factor of uncertainty),
have been erased. Statistically, most dam incidents and failures
occur during first reservoir filling or shortly afterwards as the
weaknesses in design and construction appear. As these uncer­
tainties no longer exist for astructure which has proved itself by
performing well, the nominal (theoretically computed) safety
factor does not have to be the same for an old and new dam.
However, in principle, the computed probability of failure
should not be allowed to be any higher for the old structure.
(This is an illustration of the inadequacy of using the conven­
tional safety factor).
The importance of past performance in the "re-certification”
process points out the essential role of continuous monitoring. It
enables the owner to document the dam's performance when the
issue of satisfying newcriteriacomes up.
A question which frequently arises for embankment dams is
how to apply new and stricter filter criteria to an existing struc­
ture. Rather than requiring the replacement of interior filters,
which may mean replacing the whole structure, the dam safety
authorities should accept other measures to make sure that the
overall dam safety level satisfies present standards. By that is
meant that the risk imposed by the old structure should not be
any higher than that for astructure satisfying the newfiltercrite­
ria. Othermeasures mayinclude:
• Reducing flow velocity through the dam and thereby reduc­
ing the probability of initiating internal erosion (see Section
5.3);
• Increasing downstream drainage capacity to handle a higher
potential leakage (see Section 5.4); or
• Improving monitoringof the dam.
It is estimated that probability of failure in many cases may
be reduced by an order of magnitude or more if proper moni­
toring is taking place, so that appropriate measures maybe taken
in time. However, as stated by Leps (1988) about the rapid fail­
ure of the Teton Dam, even extensive instrumentation could
probably not have provided any useful timely warning because
there was no second line of defence (see Section4.1).
8 THEDEBATEABOUT DAMS AND SUSTAINABLE
DEVELOPMENT
It is not appropriate to finish this contribution on dam engi­
neering without referring to the intense debate that has been tak­
ing place in recent years - and which will go on. At the time
Terzaghi worked with dams for development projects around the
world, there was little concern about the disbenefits dams may
create. The benefits were considered so overpowering to the
country andregion at large, that anyrequireddisplacement of lo­
cal people and any negative local ecological effects were "ac­
cepted". That is no longer the case as rigorous studies are re­
quired, and all options considered, before it is decided that dam
building is the best alternative to satisfy the needs in question.
Table 6 shows the different functions of the world’s large
dams (ICOLD, 1998). Very many dams are multi-purpose serv­
ing more thanone function. Proponents maintain that dams have
generally performed very well as an integral part of water and
energy resource development strategies in over 140 nations and,
with some exceptions, have provided an indispensable range of
water and energy services. Opponents contend that better,
cheaper and more benign options exist and have frequently been
ignored.
Table 6. Functions of the world's large dams
Irrigation 48%
Electricity generation 20%
Water supply 15%
Flood protection/control 8%
Recreation and improved environment 4%
Inland navigation 2%
Fish breeding 2%
Fire fighting and miscellaneous 1%
ICOLD (1997) has set down its guidelines, and a recent exten­
sive study initiated by the World Bank and the World Conserva­
tion Union, concludes that (WCD, 2000):
• Dams have made animportant and significant contribution to
humandevelopment, and the benefits derived fromthemhave
been considerable.
• In many cases an unacceptable and often unnecessary price
has been paid to secure those benefits, especially in social and
environmental terms, by people displaced, by communities
downstream, by taxpayers andby the natural environment.
• Lack of equity in the distribution of benefits has called into
question the value of many dams in meeting waterandenergy
development needs when compared with the alternatives.
• By bringing to the table all those whose rights are involved
and who bear the risks associated with different options for
water and energy resources development, the conditions for a
positive resolution of competing interests and conflicts are
created.
• Negotiating outcomes will greatly improve the development
effectiveness of water and energy projects by eliminating un­
favourable projects at an early stage, and by offering as a
choice only those options that key stakeholders agree repre­
sent the best ones to meet the needs in question.
Looking ahead, people will continue to build dams for many
purposes, especially in the developing world. The reason is that
dams in very many cases will bejudged to represent the best op­
tion among the feasible alternatives to satisfy critical human and
societal needs. However, a more systematic procedure of option
assessment should be developed and practised, to facilitate the
decision making.
As the world population continues to increase in water-scarce
regions and concentrate in mega-cities, additional water re­
sources must be developed. The only practical way to achieve
this on the scale required is to increase storage capacity.
With our increased knowledge and understanding, the dams
will be made socially equitable and environmentally sustainable
through stakeholder involvement, monitoring and continuous
evaluation.
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2504

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Embankment dam engineering,

  • 1. INTERNATIONAL SOCIETY FOR SOIL MECHANICS AND GEOTECHNICAL ENGINEERING This paper was downloaded from the Online Library of the International Society for Soil Mechanics and Geotechnical Engineering (ISSMGE). The library is available here: https://www.issmge.org/publications/online-library This is an open-access database that archives thousands of papers published under the Auspices of the ISSMGE and maintained by the Innovation and Development Committee of ISSMGE.
  • 2. E m b a n k m e n t-d a men g in eerin g ,s afetye v a lu a tio na n du p g ra d in g C o n c ep tio nd esb arrag esenrem b lai, év alu atio nd elas éc u ritéetam élio ratio n K .H ô e g- Norwegian Geotechnical Institute (NGI) and University of Oslo, Norway ABSTRACT: The safety and performance of adamis inseparable fromthe capacity of its foundation. A briefreview is made of Ter- zaghi’s involvement in embankment dams. The lessons learned and the state of the art are discussed together with statistics on dam incidents and failures. The safety record for tailing dams is not satisfactory and must be improved by getting more damengineering know-how into the design and construction of these types of structures. The principle of designing to provide defence in depth with “belt and suspenders (braces)” is an essential consideration. The tasks of performing safety evaluation, risk analysis and remediation of ageing dams are as challenging as the original damdesign and construction. In addition to required rehabilitation, many dams re­ quire upgrading to resist higher flood levels, stronger earthquakes and more stringent safety criteria than those applied at the time of design and construction. The paper concludes by emphasizing the need for safety legislation, damengineering education, and careful planning ofdams to support sustainable development. RÉSUMÉ: La sécurité et le comportement d'un barrage est inséparable de la capacité de sa fondation. L'article fait d'abord un court résumé des travaux de Terzaghi sur les barrages en remblai, discute les leçons importantes apprises et l'état de l'art aujourd'hui et pré­ sente quelques statistiques sur les incidents et ruptures de barrages. Les barrages bâtis avec résidus miniers n'ont pas uncomportement satisfaisant aujourd'hui. Ces barrages peuvent être améliorés par l'introduction du savoir-faire de l'ingénieur dès leur conception et construction. Une conception avec le principe “belt and suspenders (braces)”est essentielle. L'évaluation de la sécurité, les analyses de risque et la rénovation des barrages anciens présentent les mêmes défis que leur conception initiale. En plus de la réhabilitation, plusieurs barrages requièrent une amélioration pour pareràdes crues plus élevées, des séismes plus violents et des critères de sécurité plus sévères qu'initialement. L'article termine sur une perspective d'urgents besoins: législation sur la sécurité, éducation plus étendue sur l'ingénierie des barrages et planification attentive des barrages étayant un développement durable et responsable de l'environne­ ment. 1 INTRODUCTION The planning, design and construction of an embankment dam represents one of the most challenging and exciting endeavours in the field of geotechnical engineering. World-wide there are approximately 30,000 large embankment dams higher than 15 m (ICOLD, 1998). They are of many different designs and rest on foundations varying fromproblem-free, virtually impervious and incompressible bedrock to geologically complex, stratified, com­ pressible, weak and pervious soil deposits. Several of them are built on pre-existinglandslides (Schuster, 2000). More than half of the dams, and by far the biggest ones, are built since 1950. However, many are more than 100 years old. The safety re-evaluation and possible strengthening of existing dams and their foundations is a challenge no less demanding than the original design and construction work. The dams were built at a time when the state of the art, based on field experi­ ence, performance observations, and geotechnical analyses, was much inferior to current level of understanding of embankment and foundation behaviour. Furthermore, the safety re-evaluation is made even more difficult by lack of adequate documentation of the original site investigation, foundation treatment, damde­ sign andconstruction. Table 1gives alisting of the highest dams inexistence. There are 10 embankment dams, all built during recent years, higher than 210 m, but 65% of all large dams registered are less than 30 m high. The highest dams may not necessarily have repre­ sented the most challenging ones as the foundation andabutment conditions, the seismicity of the region, and the availability of suitable embankment construction materials significantly influ­ ence the degree of difficulty in achieving asuccessful result. The safety and performance of adamis inseparable fromthecapacity ofits foundation. Table 1. World’s highest dams Name Country Height (m) Dam type Rogun Tadjikistan 335 Embankment * Nurek Tadjikistan 330 Embankment Grande Dixence Switzerland 285 Concrete (arch) Inquiry Georgia 272 Concrete (arch) Vajont Italy 261 Concrete (arch) Manuel M. Tones Mexico 261 Embankment Alvaro Obregon Mexico 260 Concrete (gravity) Mauvoisin Switzerland 250 Concrete (arch) Mica Canada 243 Embankment Alberto Lleras C. Colombia 243 Embankment Sayano- Russia 242 Concrete (arch) Shushenskaya Ertan China 240 Concrete (arch) La Esmaralda Colombia 237 Embankment Kishau India 236 Concrete (gravity) Oroville USA 235 Embankment *underconstruction The following presentationis given under the headings: • Terzaghi andembankment dams • State ofthe art • Statistics on damincidents andfailures • Performance evaluation, safety assessment andremediation • Systematic riskanalyses • The need fordamsafety legislation and damengineering edu­ cation • The debate about dams andsustainable development 2491
  • 3. 2 TERZAGHI AND EMBANKMENTDAMS There is little mention of embankment dams as such in Ter- zaghi’s classical and remarkable book “Erdbaumechanik auf bodenphysikalischer GrundlageT, written here in Istanbul in 1924. In the last article entitled “Earth as building material”, he briefly discusses hydraulic fill dams, the grain size distribution in the core, the compaction of the core material andthe analyses of stresses in the core. Terzaghi was early very much aware of the possibility of soil erosion leading to piping, which was among the first subjects of his experimental investigations at Robert College inIstanbul. Already in 1922 he hadpublished his findings and secured a patent on inverted filters for the protec­ tion against failure by piping in soil foundations for concrete dams. During the following years Terzaghi recognized more and more clearly that the safety of dam foundations with respect to piping depends to a large extent on minor geological details of the subsoil, and in 1929 he published his by now classic paper “Effect of minor geological details on the safety of dams”. T T iis contribution highlighted the uncertainties that are an essential part of geotechnical practice and, as noted by Terzaghi (1961), led to the articulation of the observational method, a philosophy andprocedure elegantly expanded upon by Peck (1969). Terzaghi considered the design of the embankment portion of the dams aproblemof secondary importance. He believed that if the subsoil conditions and the pattern of seepage were reliably known in advance of construction, the stability problems could usually be solved with adequate approximation by theory, on the basis of theresults of laboratorytests (Bjerrumet al., 1960). This attitude is reflected in his selection of projects on which he co­ operated. During his professional career he was associated with the design, or with the design andconstruction ofabout 30 earth- or rockfill dams. Practically all these dams, except the earliest ones, are located on subsoils with an erratic pattern of stratifica­ tion, precluding areliable forecast of the pattern of seepage prior to construction. The Vermilion Dam, California (Terzaghi and Leps, 1958), the Cheakamus Dam, British Columbia (Bjerrumet al, 1960), and the Mission Dam, British Columbia (Terzaghi and Lacroix, 1964) are representative of the types of projects that aroused Terzaghi’s interest. The reading of these papers is a must for adamengineer. In the first edition of “Soil Mechanics in Engineering Prac­ tice” (Terzaghi and Peck, 1948) there is a chapter on dams with much emphasis on damfoundations and the danger of piping. In the preface to the second edition, which appeared in 1967 four years after Terzaghi’s death, Peck writes that Terzaghi had “added extensively to the articles on dams and their foundation. Since dams occupied an increasingly larger portion of his activi­ ties during his lateryears, these additions maybe regarded as the essence of his experience andthoughts on the subject.” The introduction to the third edition of “Soil Mechanics in Engineering Practice” (Terzaghi, Peck and Mesri, 1996), says that: ”...every statement and conclusion, pertaining to soils in the field involves many uncertainties. In extreme cases the con­ cepts on which adesign is based areno more thancrude working hypotheses that may be far fromthe truth. In such cases the risk of partial or total failure can be eliminated only by using what may be called the observational procedure. This procedure con­ sists of making appropriate observations soon enough during construction to detect any signs of departure of the real condi­ tions from those assumed by the designer and of modifying ei­ ther the design or the method of construction in accordance with the findings.” The engineeringjobs that tested Terzaghi’s insight in his ma­ ture years were mainly the water and power projects in the gla­ ciated mountains of California, and especially British Columbia (Goodman, 1999). Terzaghi is quoted as saying that the design and construction of Mission Dam was the most difficult and most daring engineering project of his entire career (Casagrande, 1964). The site is underlain by two very pervious aquifers, and underthe major portion of the damthese are separated by athick stratumof weak and highly compressible clay. Adeep grout cur­ tain through the lower aquifer, extending to amaximumdepth of about 170 m, and a sheet pile cut-off through the upper aquifer control seepage through the foundation. The nature of the avail­ able construction materials and the anticipated large differential settlements (up to 5 m) led to the design of a zoned type of em­ bankment dam. The low shear resistance of the clay stratumre­ quired that the damhave a very gentle upstreamslope. The high compressibility of the clay stratum made it necessary to design the damin such a way that the highest portion would be under­ lainonly by coarse-grained sediments in order to avoid excessive settlement of that portion. The dam incorporates the very first major use of a plastic membrane (geomembrane) over a portion of the clay blanket on the upstreamslope. The membrane, which lies under a protective cover of earth fill, was put in as an extra line of defence in case the clay blanket should crack due to ex­ cessive differential settlements. The design, construction and surveillance of Mission Dam turned out to be Terzaghi’s last job, and the famous paper by Terzaghi and Lacroix (1964) was published after his death with the assistance of careful reviews by his wife Ruth Terzaghi and Arthur Casagrande. At a special session in memory of Terzaghi that opened the Sixth International Conference on Soil Mechan­ ics and Foundation Engineering, Montreal (1965), the British Columbia Hydro and Power Authority renamed Mission Dam theTerzaghi Dam. 3 STATEOFTHEART It is not the ambition of this contribution to give a comprehen­ sive review of the state of the art of the engineering of embank­ ment dams and their foundations. Only a few aspects will be touched upon in the following sections pointing to challenges in the years to come. However, some of the more important general literature references are singled out and listed below. ICOLD (International Commission on Large Dams) was founded already in 1928 and organizes aworld congress every 3 years. For each congress four specific topics (questions) are se­ lected for discussion resulting indetailed proceedings, usually in five separate volumes. In addition, ICOLD publishes each year several bulletins (state-of-the-art guidelines) based on the work inICOLD’s manytechnical and special committees. A limited number of textbooks exist, andthere are some valu­ able books compiled from contributions at workshops and spe­ cial symposia (complete information in reference list): • Sherardet al., 1963 “EarthandEarth-RockDams”. • Hirschfeld and Poulos (editors), 1973 “Embankment-Dam Engineering”Casagrande Volume. • US National Research Council, 1983 “Safety of Existing Dams". • Cooke and Sherard (editors), 1985 “Concrete Face Rockfill Dams”. • Leonards (editor), 1987 “DamFailures". • Jansen (editor), 1988 “Advanced DamEngineering”. • Neves (editor), 1991 “Advances in Rockfill Structures”. • Kjæmsli et al., 1992 “Rockfill Dams - Design and Construc­ tion”. • Fell, MacGregor and Stapledon, 1992 “Geotechnical Engi­ neering of Embankment Dams”. • Singh and Varshney, 1995 “Engineering of Embankment Dams”. • Terzaghi, Peck and Mesri, 1996 “Soil Mechanics in Engi­ neeringPractice”. It should be noted that in several of thebooks listed above by the names of their editors, there are excellent contributions (chapters) by some of the outstandingengineers in the field. T T ie central role of the topic of embankment dams and their foundations in geotechnical engineering is demonstrated by the many Rankine and Terzaghi lectures on various aspects of the 2492
  • 4. subject (e.g. Casagrande, 1961; Newmark, 1965; de Mello, 1977; Seed, 1979; Cook, 1984; Penman, 1986). RalphPeck presenteda lecture in 1979, which he entitled “Where has all thejudgement gone”(Peck, 1980). Since then he has repeatedlyreturnedtothis theme, and below is anexcerpt fromthat paper; mainly referring toembankment dams: .... A failure is seldom the consequence of a single short­ coming. Usually there is at least one other defect or deficiency, and the failure occurs where two or more coincide. This infer­ ence supports the principle of designing to provide defence in depth, the “belt and suspenders”principle long advocated by Ar­ thur Casagrande. It postulates that if any defensive element in the damor its foundation should fail to serve its function, there must be one or more additional defensive measures to take its place. Teton Dam is an outstanding example of violation of the principle; the sole line of defence was the core andgrout curtain. Under such conditions, it is almost irrelevant to define the pre­ cise manner in which the failure started or whether there may have been such deficiencies in construction as awet seamacross the core. The design should have provided adequate defences against anysuch defect. The bedrock treatment appropriate to the geological condi­ tions is amatter of design. It is not an aspect of design suscepti­ ble, however, to numerical analysis. Instead, it requires the exer­ cise ofjudgement, a sense of proportion. Whenjointed bedrock foundation is being treated and covered with the first layers of fill - acrucial time with respect to the future performance of the dam- engineers fully acquainted with the design requirements should be present, should have the authority to make decisions on the spot, and should not delegate their authority unless and until they are satisfied that theirjudgement concerning the par­ ticular project has been fully appreciated by their subordinates. I doubt if guidelines, regulations, or even the best of specifi­ cations can take the place of personal interaction between de­ signers and field forces at his stage. Frequently, as a consultant or as a member of a board of consultants, I have walked over a recently exposed foundation or abutment with the field forces, discussing place by place what treatment would be appropriate. Together we studied details of foundation conditions, observed treatment in progress, agreed upon orchanged it. Inthis manner, the consultants evaluated the potential problems and their solu­ tions, and the field forces gained the necessary insight as to what was required. The type of foundation treatment is not a matter to be deter­ mined by ageologist, unless he is truly anengineering geologist. The geologist should investigate the geological characteristics of the foundation and its interface with the dam and make them known to the engineer who will form thejudgement concerning treatment. The consequences of the flow of water near the inter­ face, including its effect on the various materials in the dam, are within the realm of the engineer and the decisions regarding treatment areengineeringdecisions. The three failures that I have discussed in some detail origi­ nated at the interface between dam and foundation. Others, that might equally have been chosen as examples, arose from over­ looking or misjudging geological features in the foundation it­ self. A few had their origin in construction defects in the em­ bankment. They had in common that all were outside the scope of numerical analyses. They would have been prevented if judgement arising fromextensive experience had been given full scope of design and construction, and if the design hadincluded multiple defences. Accordingly, I think it quite possible that the incidence of failure of major dams could be reduced an order of magnitude by focusing attention on the details of design and construction that cannot, at least presently, be covered by analy­ sis, that perhaps cannot beknown until construction is underway, but that require the personal attention of experienced engineers. Research should be directed to those aspects of design and con­ struction in greatest need of improvement; definition of founda­ tionconditions; conditions conducive to internal erosion and the means for controlling it; filter criteria and their practical achievement in construction; prevention and treatment of crack­ ing. The goal of the research should be improved understanding, preferably but not necessarily quantitative. The literature already has much to say about cracking of earth dams. The emphasis, however, is on the mechanics of producing the initial cracks, an aspect that has recently become at least partly amenable to analysis. The analytical results serve auseful purpose; reduction of cracking can undoubtedly be achieved most successfully if the causes of cracking are understood and avoided. Nevertheless, to accord with the principle of defence in depth, every damshould be designed on the assumption that the core maycrackand that thedamshould be safe even if it does. So we reckon with the conclusion that modem dams seldom if ever fail because of incorrect or inadequate numerical analy­ ses. They fail because inadequate judgement is brought to bear on the problems that, whether anticipated or not, arise in such places as the foundation or the interface between embankment andfoundation. Sometimes they disclose themselves only in sub­ tle ways in theuse of the observational procedure. Irrespectiveof specifications, contractual arrangements, possibilities of claims for extras, or delays, these problems must be recognised and solved satisfactorily....... 4 STATISTICS ON DAMINCIDENTS AND FAILURES Some very informative descriptions and discussions of embank­ ment damfailures are presented by Sherard et al., (1963) and in the books edited by Leonards (1985), Singh and Varshney (1995), andJansen (1988) where lessons fromnotable events are presented. Table 2 shows examples of recent ICOLD conferences and publications on the subject of safety, reliability andrisk. ICOLD (1995) provides a world-wide review (except China) including 52 concrete and 129 embankment dam failures and their causes. This review shows clearly that failures, when they occur, mainly take place very early in a dam’s life. Table 3 summarizes the specific information on the causes of failure for the embankment dams considered in the study, includingfailures during construction. The information presented in Table 3 corresponds with the results inTable 4 fromaprevious study of incidents and failures registered for 240 embankment dams in the USA (USNRC, 1983). As can be seen fromboth tables, internal erosion consti­ tutes a prim arycause of concernand will bediscussedin Section 5. A closer study shows that the incidence of piping through the embankment is about two times higher than piping through the foundation. Table 2. Recent ICOLD events focusing on dam safety 1993 “International Workshop on Dam Safety Evaluation", Grindelwald, Switzerland. 1994 “Safety Assessment and Improvement of Dams", ICOLD Congress, Question 68, Durban, South Africa. 1995 “Dam Failures - Statistical Analysis”, ICOLD Bulletin 99. 1996 “Current Issues and Advances in Dam Safety”. Interna­ tional Conference, Ontario, Canada. 1997 “Incidents and Failures of Dams”, ICOLD Congress, Ques­ tion 75, Florence, Italy. 1997 “Risk-Based Dam Safety Evaluation’’, International Work­ shop, Trondheim, Norway. 1998 “Managing the Risks of Project Development, Safety and Operation”. International Conference, Buffalo, New York, USA. 1998 “New Trends and Guidelines on Dam Safety", Interna­ tional Symposium, Barcelona, Spain. 2000 "The Use of Risk Analysis to Support Dam Safety Deci­ sions and Management", ICOLD Congress, Question 76, ___________ Beijing, China._________________________________________ 2493
  • 5. Table 3. Primary causes of embankment failures or partial failures (ac­ cording to ICOLD, 1995) Causes of failure TE ER ER/TE (% ) (% ) (% ) Overtopping (of crown) 23 45 31 Internal erosion (piping) - in dam body 20 8 23 Internal erosion (piping) -in foundation 13 13 15 Other structural causes - e.g. slope instability and 29 25 23 settlements Other causes 15 9 8 Total (percentage) 100 100 100 Total number of dams 92 24 13 TE= Earthfill; ER= Rockfill Table 4. Causes of embankment incidents and failures according to US- COLD (USNRC, 1983) Causes of incident or failure % of 240 dams External erosion (overtopping/wave action) 29 Internal erosion (in dam body/foundation) 38 Foundation instability 14 Excessive dam deformation 13 Deterioration (chemical/physical) 2 Malfunction of gate 2 Earthquake effects 1 Construction errors 1 The experience with the 175 large embankment dams in Nor­ way, the highest being 145 m, is described by Kjaemsli et al. (1992) and Hfleg et al. (1993). Most of these are rockfill dams with a broadly graded moraine core, but several of the recent ones have asphalt concrete core (Hfieg, 1993; 1998). There has been no failure of an embankment dam in Norway higher than 15 m, but of the 175 built, 32 have had some repair. Twenty have sustained minor damage to their upstreamslope protection as aresult of wave and ice action. Six have suffered some inter­ nal embankment erosion, in two cases probably preceded by hy­ draulic fracturing, and six have been affected by excessive or differential settlement. A 10m high earthfill dambuilt in 1975 failed in 1976 as aresult of erosion along aconcrete culvert go­ ing through the moraine core - ingeneral, avery poordesign fea­ turewhich should be avoided. Remedial work in Norway has consisted of improved rip-rap design and construction, and internal erosion and leakage have been controlled with water-cement-bentonite-sand mixture grout injection. Of all the dams completed since 1976, only one has required repair, demonstrating that lessons have been learnt from the experience gained, and thatthere have been improvements in design criteria andconstruction andcontrol procedures. In summary, areview of the available statistics fromdifferent parts of the world and accompanying evaluations and analyses (for example Londe, 1993; ICOLD, 1995; ICOLD, 1997; Foster et al., 2000a) show that the causes of damincidents and the fre­ quency of failure vary fromone region to another. However, the average probability of failure per dam-year has been reduced from around 10" 4 towards 10'5over the last 30 years. Further­ more, adambuilt some 30 years ago and still performing well is as safe as a dam built with today’s state-of-the-art technology andquality control. In general, but excluding tailing dams, the safety record for dams is good and it is steadily improving. However, there is no room for complacency because we have had incidents and fail­ ures even with dams built during recent years (e.g. Teton Dam, 1976; Gouhou Dam, 1993), and continuous monitoring and maintenanceof existing dams is mandatory (see Section 5). As part of the US National Dam Safety Program, a National Performance of Dams Programhas been established. The aimis to ensure that safety related dam incidents and failures be re­ ported to a common information centre at Stanford University, California. This will allow dam engineering and safety profes­ sionals to benefit from the lessons of in-service dam perform­ ance across the USA. It will further increase the probability of including all potential incident and failure modes in future risk analyses (see Section 6). Othercountries orregions should estab­ lish similar programs, because incidents do occur, but many are not properly reported and analysed. 4.1 The cases of Gouhou Dam and Teton Dam The failure during first reservoir filling of the 71 mhigh Gouhou concrete face embankment dam, built in China in 1993, is de­ scribed by Chen (1993). Almost all modem concrete face em­ bankment dams are built of sound rock materials, while Gouhou Dam consisted primarily of sandy gravel. When leakage devel­ oped through the concrete facing, pore pressures built up in the sandy gravel in the downstream shoulder as the drainage provi­ sions were inadequate (see Section 5.4). The cross-section de­ sign and zoning did not adequately take into account the differ­ ences in material properties and behaviour between a good rockfill, with gradually increasing rock size towards down­ stream, and the sandy gravel which was used. This led to the complete damfailure when cracks developed in the concrete fac­ ing. Experience shows that opening ofjoints or cracks often oc­ curs in concrete facings and must be allowed for in the safe de­ sign ofthis type ofdam. Teton Dam, Idaho, 93 m high, was built in a steep walled canyon incised by the river into the Texburg Bench. The rocks exposed in the canyon walls are almost entirely of volcanic ori­ gin. At the dam site, they consist primarily of intensely layered andjointed rhyolite with minor inclusions of basalt, breccia, and welded ash-flow tuff. The embankment was built mainly of the locally available silt material. Failure occurred during first filling of the reservoir in June 1976. Leps (1988) states that the lessons learned clearly do not represent new lessons for the profession, but serve as essential reminders of points sometimes ignored orforgotten. a) The responsible design engineer should be required to visit the construction site, perhaps monthly, to verify that site con­ ditions and construction materials conformto the design con­ cept and, if not, to determine required modifications. b) The downstream contact of animpervious embankment zone, whether against foundation materials or against amore pervi­ ous embankment zone, must be protected against piping by use ofengineeredfilter zones. c) Ingrossly pervious foundation bedrock, asingle grout curtain should not be reliedupon to be adequately effective. d) Whenever impervious borrow exists at moisture contents se­ verely below optimum, it should be mandatory initially to moisture-condidon the material to near optimum, first in the borrow area and thereafter, but to avery minordegree, on the fill. e) Deep, narrow, key trenches in bedrock, with steep side slopes, should be avoided because they invite arching of backfill as it settles, and thereby establish unfavourable stress conditions that are conducive to hydraulic fracturing. f) Because of inevitable hydrologic uncertainties, and difficul­ ties in forecasting precisely when critical water control out­ lets may be completed and serviceable, it is frequently almost academic to assume that it will be possible to control the rate of initial reservoir filling. Hence, the dam designer should fully consider that the reservoir may fill very quickly, regard­ less of the generally assumed merit of controlling the filling rate. g) It is unlikely that, even if extensive instrumentation had been provided, any useful timely warning of impending failure would have been sensed and evaluated in advance of the sud­ den, veryrapidfailure ofTeton Dam. 4.2 The case ofmine tailing dams Mine tailing dams are not included in the surveys and statistics referred to above. They show a relatively poor safety record, which must be improved by getting more dam engineering 2494
  • 6. know-how into the design and construction of these types of structures built by the mining industry (ASDSO 2000b). Morgenstem (1998, 2000) refer to eleven serious incidents over the short period 1995-1998 associated with mine tailings and waste overburden management, and several incidents and fail­ ures have occurred since that time. Morgenstem states that all were modem structures and “were not part of the historical leg­ acy of poorly engineered waste containment structures that char­ acterized parts of the miningindustry in the past”. Clearly the state of the art and practice for these types of pro­ jects is not satisfactory, and recent efforts by ICOLD, the UNDP and the mining industry have increased the awareness of this situation. 5 PERFORMANCEEVALUATION, SAFETY ASSESS­ MENT AND REMEDIATION The ageing dampopulation requires regular maintenance andre­ habilitation (e.g. Penman and Milligan, 1993). In addition, strengthening may be required to satisfy current safety and risk criteria based on state-of-the-art knowledge. Society will have to spend significant resources in the years to come to ensure thede­ sired performance and safety of our dams. In recent surveys by ASCE (1998) and ASDSO (2000a) the latter estimates that US$ 40 billion is needed to properly rehabilitate and upgrade dams in the USA. In general, embankment dams have shown to be very resis­ tant to earthquake shaking. However, due to the potential lique­ faction hazard for old hydraulic fill dams and dams resting on loose alluvial foundations, strengthening has been found advis­ able in a number of cases (e.g. Seed, 1979; Marcuson et al., 1994; Finn, 1996). The case study presented by Gillon et al. (1998) for the extensive upgrading of Matahina Dam, New Zea­ land, is most informative. However, this topic will not be further addressed herein. Quite often the reasons for excessive leakage, internal ero­ sion, excessive displacements, differential settlements or crack­ ing in an embankment dam may not be obvious. Careful inter­ pretation of observations, visual and through field instruments, must be carried out to assess the situation before specific meth­ ods of repair or upgrading are decided upon. Unexpected obser­ vations may not give any reason forconcern if alogical explana­ tion can be found. Three questions should be answered during the evaluation: • What is “abnormal” embankment behaviour? • Does the deviation from predicted behaviour indicate lower safety than aimed forin the design? 1 = moraine core; 2 = sandy gravelfilter; 3 - transition rockfill; 4 = supporting rockfill; 5 - slope protection 6 =protective cap ofselected blocks: and 7 = grout curtain • Does thedeviation require remedial action? In the following sub-sections, four aspects of embankment dam behaviour are considered. They illustrate the need for cor­ rect interpretation of observations before the diagnosis is given anddecisions are made how to remediate. 5.1 High pore pressures in the earth core In several embankment dams with earth core, the measured pore pressures in the downstream portion of the core have been re­ portedto be much higher than predicted duringdesign. Two well documented studies are the Svartevann Dam, Norway (Kjaemsli et al. 1982; DiBiagio et al., 1982) and the WAC Bennett Dam, British Columbia (Stewart and Imrie, 1993). Did the high pore pressures indicate that critical cracks or “channels” had devel­ oped through the core? Figure 1shows the maximumcross section of the 129 mhigh Svartevann rockfill dam with a slender and inclined broadly graded moraine core, founded on bedrock. Figure 2 shows the measured piezometric heads versus reservoir level in three pie­ zometers at el. 810 located in the core upstream, in the centre and downstream, respectively. In total 24 electric closed-system piezometers (vibrating wire) were located in this same core cross-section. Piezometer P12 gave readings that consistently fall on the 45° line in Fig. 2, showing that the measured pore pressure close to the upstream face of the core was equal to the water pressure in the reservoir at that level. During the first year, piezometer P14 showed much higher pore pressures than those predicted based on conventional theory of saturated steady-state flow. However, after two full cycles of seasonal lowering and raising of the reservoir, the piezometric head in P14 had de­ creased significantly, approaching the theoretical solution. Fig­ ure 3 shows the piezometric head versus time for PI2, PI3 and P14 up until 1989, 13 years after end of construction. The reser­ voir level at any given time is that recorded by piezometer PI2. Equilibrium has been reached, and there is no further reduction in the pore pressures on the downstream side, as P14 only re­ flects the changes in reservoirlevel. S i i4»i i '« J i ' 1 f •1.774.5 JUjlg M 1^ w rw ^T U 'ja J W ffT T O 0 100 m The Svartevann rockfill dam during construction. Vatnedalen Damin Norway (125 m) shows similar trends forthe measuredpore pressures (Myrvoll et al, 1985), as well as several other dams described in the international literature. Many hy­ potheses have been proposed over the years, and the following are some of the explanations presented for the unexpected pore pressures: Figure 1. Cross-section and photo of the Svartevann Dam, Norway. 2495
  • 7. R *s»rvouw atmta v eltm l Figure 2. Measured piezometric heads versus reservoir level from 1975-1979 for Svartevann Dam. (i) Heterogeneities, construction imperfections and larger hori­ zontal than vertical permeability are not properly considered in the prediction analyses. Therefore, the downstream pore pressures are underestimated. (ii) Excess construction pore pressures remain in the core for a longer time thanpredicted. (iii)A lower permeability coefficient on the downstream side as aresult of higher effective stresses thanon the upstreamside (deMello, 1980; Vaughan, 1989). (iv)Cracks initiated by hydraulic fracturing caused by arching effects and locally lowered effective stresses in the core (for example Sherard, 1984; 1986; de Fries, 1991). Pore pressure communication through the cracks gives high pore pressures downstream. (v) Migration of fines from the core to the downstream filter, which becomes “clogged”. There will then be overpressures in the downstreamportion compared with those predicted in a conventional analysis (Peck, 1990; Stewart and Imrie, 1993). A satisfactory hypothesis or combination of hypotheses must not only be able to explain the high temporary pore pressures downstream, but also the decrease that has been measured with time. Since the presentation of the “abnormal” pore pressure ob­ servations fromthe Svartevann and WAC Bennett dams, Hydro- Québec (Canada) has reported several similar cases. First St- Amaud (1995) and then Dascal (1995) offer the following ex­ planation: (vi)After compaction, the material in an earth core is usually not saturated (typically 50-90 percent). —During reservoir impoundment, air (gas) is trapped in the submerged zones. The pressure measured by closed- system piezometers in partly saturated soils is the air pore pressure, which, in general, is higher than the pore water pressure. —The permeability coefficient upstream increases as the air bubbles are dissolved or transported down stream. —The pore pressures decrease, and therefore the volume of free gases increases in the direction of flow. Furthermore, dissolved gases in the waterupstreamcome out of solution towards downstream. Thus, the degree of saturation and core permeability decrease towards downstream. —This contrast in permeability, which can be quite sig­ nificant, causes pore pressures downstream which are much higher than those predicted from a seepage analysis for ahomogeneous core. —Some blockage of the flow will exist as long as free gases are present. Reaching full saturation and steady state flow may take a long time. Until then, there will be pore over­ pressures in the downstreamportion of the core. There will not be one hypothesis which satisfactorily explains all cases and situations encountered or reported in the literature. However, explanation (vi) seems well founded, and may apply to many dams, e.g. Svartevann, where cracking, erosion and trans­ portation of fines are not the reasons for the unexpected pore pressurebehaviour. At Svartevannthe decrease in measured pore pressures started after only a short time, while at WAC Bennett it took several years before the trend turned (Stewart and Imrie, 1993). Further theoretical and experimental studies sponsoredby Hydro-Québec andothers have recentlybeenundertaken to more fully understand and test the hypothesis presented by St-Amaud (1995), and they support the concept (CGS, 2000). High down­ stream pore pressures due to this phenomenon will not require remedial work, while internal cracking and crack erosion may call forrehabilitation by grouting orother measures. 5.2 Large post-construction displacements Pore pressures and displacements measured during embankment construction give information about the deformation properties of the foundation and of the materials compacted in the different embankment zones. The measurements are of value when pre­ dicting displacements caused by further embankment construc­ tion and reservoir filling, and post-construction movements with time. Post-construction displacements of large dams are usually 900 880 860 340 / Y U ■ ( v 4 y V V / s / 4 I j * 9 P12 y V V * r V N s ' s y y v V A P13 / [ / ÿ v V V V V V V /- v y V i i j V — •*— * v __ — - P14 rfSB S? 820 800 780 1974 1875 1978 1977 1878 1379 1880 1381 1982 1983 1984 1985 1988 1987 1988 Ì989 E n do!contract»» T imtly.*(| Figure 3. Measured piezometric heads versus time from 1973 to 1989 for Svartevann Dam 2496
  • 8. measured, at least at the crest, while measurements in the interior are more rare. The magnitude and rate of post-construction dis­ placements are often taken as anindication of the “health”of the embankment by comparing with corresponding measurements fromotherstructures reported in the literature. When this is done, and to evaluate whether the displacements are abnormal or not, it is important to specify the location of each measurement point and the time of the first measurement after end of construction (that is, the reference value for subse­ quent measurements). It is not uncommon for the vertical dis­ placement component of the upstream crest bolt to be signifi­ cantly larger than the settlement of the corresponding downstream crest bolt. This is primarily caused by the raising of the reservoir, especially the last 30 per cent up to the maximum level, unless the reservoirhas been filled simultaneously with the embankment construction. Inseveral cases, the increased compressibility andsubsidence of the upstream shoulder on submergence has caused a relative slip between the fill and the core in the upper part of the em­ bankment. This results in differential settlements across the crest and possibly longitudinal cracks along it. The phenomenon is of no real concern with respect to dam safety, as the movements stabilize after the first reservoir filling, lowering andrefillingcy­ cle, and cause no transverse cracks. The observation does not call for a flattening of the upstreamslope, but possibly some re­ pair to the rip-rap protection (e.g. Paré, 1984; Hóeg et al, 1996). Table 5 gives the measured post-construction crest settle­ ments (upstream, top of thecore anddownstream) forsome large Norwegian rockfill dams built since 1972 on stiff foundations. The dams above the double horizontal line in Table 5 have cen­ tral or gently sloping clay moraine core, while the dams below have thin asphalt concrete core. It can be seen that the Vatneda- len I and Deg dams have very small core- and downstream set­ tlements, but fairly large upstream settlements. This is because of the rockfill saturation effect described above, resulting in lo­ cal subsidence in the top part of the upstream slope. The up­ stream slope for the Vatnedalen dams is 1V:1.5H and for Deg dam 1V:1.6H. Table S. Post-construction settlements for Norwegian rockfill dams on stiff foundations Dam Year H (m) Vertical settlements (%H) Crown Top Crown upstream core down­ stream Oddatj0m 1987 145 0.26 0.20 0.22 Svartevann 1976 129 0.80 0.80 0.65 Vatnedalen I 1983 125 0.90 0.20 0.27 Deg I 1972 90 0.70 0.15 0.15 Nyhelleren 1979 85 0.12 0.12 0.12 Vatnedalen II 1983 60 0.10 0.10 0.10 Juklal 1973 59 0.60 0.65 0.33 Storvatn 1987 90 - 0.20 - Berdalsvatn 1988 65 018 0.14 0.10 Styggevatn 1989 52 0.12 0.20 0.10 Riskallvatn 1986 45 0.20 0.15 0.10 Storglomvatn 1997 125 0.20 0.16 0.11 Figure 4 gives a simplified overview of the measured post­ construction crest settlements for rockfill dams worldwide, built on stiff foundations. The data have been collected from several authors (Soydemir and Kjaemsli, 1979; Clements, 1984; Dascal, 1987; andHOeget al., 1996), and the scatteris significant. Inthe literature it is not always indicated where across thecrest the set­ tlements are measured (upstream or downstream). Most rockfill dams built of sound rock since 1970 show a trend that gives a post-construction crest settlement in the range of 0.2-0.4% of the maximumdam height after 25 years of operation. The trend is approximately linear with the logarithm of time, and there is no clear indication that high dams give a higher normalized set­ tlement than lower dams. Some modem dams are reported to have settlements considerably larger than those indicated above. but no satisfactory explanations have been presented. For older dams, built mostly without rockfill compaction, the normalized post-construction settlements are considerably larger and the scatterin the results much greater (Fig. 4). Post-construction displacements of dams on stiff foundations dependon many factors, including; — properties of rockfill andcore materials; — layer (lift) thickness andcompaction effort; — sluicingof rockfill during placement; — steepness of exterior slopes; — shape of valley; —upstreamimpervious face orcentral core; — zoning ofembankment; — otheraspects. However, some important factors are sometimes overlooked when displacements are evaluated and compared with corre­ sponding measurements from other embankment dams. These are: — the location of points on the crest where measurements are taken; — time of first crest measurements after the completion of con­ struction (a significant part of the long-term settlement takes place during the first few months); — reservoir level at the end of construction when crest settle­ ment bolts were installed; — rates of damconstruction andreservoir filling; — magnitude of reservoirfluctuations. These aspects make it difficult to make “fair” comparisons such as those proposed in Table 5 and Fig. 4, but the factors must be considered before onejudges whether the recordedpost- constructiondisplacements are “abnormal” or not. If, in addition, the damsits on an inhomogeneous and compressible foundation, the comparisons are that muchharderto make. 5.3 Internal erosion - will dam selfheal? As presented in Section 4, many incidents andfailures havebeen attributed to internal erosion. Our concern has grown in recent years as it has been clearly documented that damaging internal Figure 4. Measured post-construction crest settlements for rockfill dams built on stiff foundations erosion may not only show up during initial filling of reservoir or shortly thereafter, but first several years later (Marsal and Pohlenz, 1972). As safety evaluation of ageing dams is receiving increased attention, so is the topic of possible internal erosion developing at a later stage in adam’ s life. Charles (1997) gives an excellent overview, and recent papers are for instance pre­ sented by Fosteret al. (2000b). 2497
  • 9. In many instances of increased leakage of turbid(muddy) wa­ ter, clearly indicating a process of ongoing internal erosion, the leakage has stopped almost as quickly as it started, returningto a normal seepage rate. Erosion “pipes” which had started to de­ velop, collapsed and closed, as the downstream filters had been working after some transport of fines from the core had taken place. It points to the essential role of proper filter design crite­ ria, which have become much stricter in recent years. Starting with the classical work by Terzaghi in the 1920s, very many en­ gineers have studied filter requirements and properties. The cri­ teria by Kenney and Lau (1985) and Sherard and Dunnigan (1989), and summarized by ICOLD (1994), represent the state of the art. There are specialty conferences regularly organized on this topic alone (Wolski and Mlynarek, 2000), and Vaughan (2000) presents recent reviews and evaluations. However, good filter design criteria by themselves are not sufficient to ensure satisfactory performance. The field placing process and control is just as important to avoid segregation and inhomogeneous fil­ ter properties leading to local weak spots which the seeping wa­ ter is sure to find. This is one of the ’’extreme value problems”; as defined by de Mello (1977), andit calls for “defence indepth” (Section 3). 5.3.1 Initiation ofinternal erosion Inadequate filters do not cause erosion, which is initiated by one of the mechanisms described below, but they fail to halt (arrest) erosion which has started and which may lead to damage oreven damfailure. Flowing water exerts drag forces on the soil particles in the direction of flow, and these drag forces increase with flow veloc­ ity. Intergranular contact stresses, interlocking and any true co­ hesion (cementation) between particles prevent themfrombeing tom loose, unless a critical flow velocity is exceeded. This criti­ cal velocity therefore depends on material properties and the lo­ cal effective stress condition. The phenomenon of mechanical internal erosion may be clas­ sified into four main categories: piping, internal mass erosion (suffusion), contact erosion andcrackerosion. However, the ero­ sion process may well start by one mechanismandgradually de­ velop into another form, e.g. start as mass or crack erosion and develop into piping. Piping is the most dangerous of the mecha­ nisms, because due to the process of backward erosion, the se­ verity of it may not be detected until the pipe (eroded canal) breaks through on the upstream side in direct contact with the reservoir. The internal erosion may also cause sinkholes on the crest or upstream slope of the dam, which in turn may lead to overtopping. The case studies reported in the literature often refer to in­ adequate filters as the cause of the incident or failure and there­ fore fail to identify the real cause oferosion initiation which may have been one ofthe following: • Unfavourable properties of core material which was easily erodible (i.e. internallyunstable), dispersive, or in some cases partlydissolved due to chemical reactions; • Inadequate core material compaction, e.g. due to unsatis­ factory quality control; • Vertical and narrow core between stiff adjacent zones which led to arching action, reduced effective stresses, hydraulic fracturingandcrackopening; • Inadequate preparation and sealing of fractured rock foun­ dation or abutment, which also may have had crack infill or wall material subject to dissolution; • Narrowcut-offtrench underthecore in inadequatelyprepared fractured rock. A trench which is too narrow may lead to arching, reduced effective stresses and erosion or hydraulic fracturing; • Embankment design not adapted to a foundation overburden with greatly varying compressibility or depths to bedrock across the valley floor. This caused differential settlements and transverse cracking or zones with very low effective stresses; • Inadequate compaction and low contact stresses against cul­ vert, sheet pile wall or concrete structure leading to contact erosion; • Design and construction not adapted to unfavourable topo­ graphy with local depressions and protrusions in foundation and abutments. This may lead to low local effective stresses and cracking. In a narrow valley one may also get significant arching between the abutments and reduced effective stresses in the lower portion of core; • Reduction in local effective stresses and cracking due to dif­ ferential displacements caused by uneven regional subsidence or fault movements; • Theory and practice indicate that the probability of crack- opening in the core increases with increasing rate of em­ bankment construction andreservoirfilling rate. There is then too little time allowed for the different embankment zones to adjust among themselves to the changing loading conditions. Recent experience has shown that earth core material around and in the vicinity of vertical instrument cables and pipes (in­ strument islands) is not (cannot) be compacted properly. This has, for instance, led to local settlements (collapse) upon wet­ ting, sinkholes, local internal erosion, internal loose zones or even cavities. This method of instrumentation must be re­ considered. Furthermore, the local observations and occurrences at such instrument islands may not give reliable indications of the well-being of the embankment in general, and incorrect con­ clusions may be drawn about thedamperformance. If properly placed, filters may prevent transportation of parti­ cles out of the core and thus arrest the erosion process that has been initiated by one of the mechanisms listed above. The design of the damand the filter zones must be such that settlements and distortions do not impair or weaken the functioning of the filters. Few, if any, of the 122 Norwegian large rockfill embankment dams with broadly graded moraine core satisfy today's strict fil­ ter criteria, which in most cases will require mechanical process­ ing of the filter material. The reason for not having experienced more than a few incidents of damaging internal erosion is that the critical flow velocity has not been exceeded, or that the fil­ ters locally have been adequate although they were not designed to satisfypresent state-of-the-art criteria. In addition to the mechanical erosion phenomenon described above, one may face the problem of dissolution (chemical ero­ sion) of the material. Incore construction one must avoid the use of materials that will be dissolved by the seeping water. One must then also consider possible changes in reservoir water chemistry with time for instance due to pollution. The presence of dissolvable materials in the damfoundation (e.g. karst) repre­ sents a more challenging task for the designer, as discussed by Jansen (1988). That may require the use of extensive and multi­ ple-rowgrout curtains orpositive cut-off walls. 5.3.2 Examples ofrecent dam cross-sections The concern about the potential hazard of internal erosion in earth cores has in some cases been the argument for choosing a design with upstreamconcrete facing or interior asphalt core, al­ though earth core material was locally available. In other cases, of course, climatic conditions and construction scheduling and duration, have been the factors which decided against the use of acompacted earthcore. The West Dam of the Eastside Reservoir in Southern Cali­ fornia is an example of a recent rockfill structure with an earth core built to high quality and state-of-the-art standards wrt. in­ ternal erosion resistance, filter design and construction (Forrest et al., 1997; ENR, 1997). Among several alternatives considered, an earth core design was selected. The earth core has a maxi­ mumheight of 102 mandthe damlength is 2,500 m. It is anoff- river reservoir built to provide emergency water supply in a strongly seismic region. Therefore, it is a conservative design with a wide core, generous fillers of processed materials and gentle exterior dam slopes. A 40 m deep cut-off wall of plastic concrete through the alluvium and keyed into bedrock virtually 2498
  • 10. eliminates foundation seepage and any possibility of internal erosion in the highly variable andinhomogeneous foundation. Figure 5 shows the cross-section design forthe modemOdda- tjttm rockfill dam (145 m high) with an earth core of broadly graded moraine (Kjimsli et al., 1992; Windisch and HOeg, 2000). The damwas completed in 1986 and is based on previous experience with many similar but lower dams in Norway. The photo shows the dam located in the Norwegian mountains to­ gether with two other dams to create the reservoir for hydro­ power. Figure 6 presents the cross-section design for a modem con­ crete face rockfill dam (CFRD), and the photo shows Foz do Areia Dam in Brazil, 160 m high, completed in 1980 (Cooke, 1998; 1999). Figure 7 presents the cross-section design for a modem as­ phalt concrete core rockfill dam (ACDR) (Hoeg, 1993) and a photo of the recently completed Storglomvatn Dam, Norway. So far this is the highest damof its kind (125 m), but several higher ones areunderconsideration. 5.4 Drainage capacity and resistance to leakage or over­ topping In the design of new embankment dams as well as in the safety evaluation of existing ones, one must assume that temporary sig- Figure 5. Cross-section of OddatjOm rockfill dam (145 m high) with inclined moraine core. Photo shows OddatjCm Dam on the left (Fjellanger Wider0e A.S.) Fac*slao 1A = Impervious soil; IB = Random fill, 0.5 m layers; 2A = Processed fine filter; 2B = Crusher-run rockfill; 3A = Selected small rock placed in same layer thickness as Zone 2; 3B = Quarry-run rockfill, about lm lay­ ers; 3C = Quarry-run rockfill, about 2 m layers; 3D = Dumped rockfill (optional). Compaction for rock zones; four passes of 1 0 1 vibratory Figure 6. Cross-section of a modem CFRD of sound rockfill on a sound rock foundation (Cooke, 1998). Photo shows Foz do Areia in Brazil, 160 m high (Cooke, 1999). 1 = asphaltic concrete core; 2 = gravel transition, 0-60 mm; 3 = crushed rock transition, 0-200 mm; 4a = rockfill, 0-400 mm 4b = rockfill, 0-800 mm; 5 = rip-rap; 6 = crown cap, large blocks 7 = toe drain, large blocks > 0.5 m3 Figure 7. Cross-section of Storglomvatn rockfill damwith vertical as it was being topped offin 1997. asphalt concrete core (ACRD). Photo shows the dam(125 mhigh) 2499
  • 11. nificant interior leakage may occur. The dam must be able to safely accommodate such a leakage until it either selfheals, the reservoir level is lowered, or remedial work is done. This re­ quires that the downstreamdrainage capacity is designed to han­ dle the leakage without the occurrence of scour and unravelling or local slope instability thatbyprogressive action mayendanger the safety of the structure. Satisfactory drainage capacity pro­ vides the second line ofdefence (de Mello, 1977; Peck, 1980). In general, rockfill dams have inherently much higher resistance than earthfill dams as they tolerate orders of magnitude larger leakage rates before afailure situation develops. A comprehensive andconcise definition of the termrockfill is difficult and varies from one country/region to another. Leps (1988) proposes that to be termed rockfill, the material must have an average particle size of at least 50 mm, and no more than 40%of the average sample should be smaller than 25 mm. Thus, a limit is imposed on the finer fraction, but no limit is im­ posed on the maximum particle size. If the percentage of minus 25 mm material exceeds 50%, that fraction will begin to domi­ nate the stress-strain and permeability properties, as it becomes the matrix that, when perfectly blended, completely surrounds and separates the larger rock particles. The result is lower shear strength and lower permeability, andthereby adiminution of the fundamental assets of rockfill. The particle size referred to is that after compaction, which may be significantly smaller than that taken out of the quarry, borrow area or tunnel excavation. The extent of crushing de­ pends on rock type, mineralogy and compaction equipment and procedure. The average gradation of a lift may be a misleading characteristic in that the fill is never perfectly blended. The coarser particles always concentrate at the bottom of each lift andthe finer constituents at the top. 5.4.1 Failure mechanisms In the safety evaluation of existing structures, one often finds that present hydrological information and design criteria lead to higher probable flood levels than the dam originally was de­ signed for. This may be due to changes in climate andincrease in precipitation levels. Therefore, the resistance of the damto over­ topping must be assessed. The remedial work may consist of dam heightening, armouring the dam crest by roller compacted concrete (RCQ, andreinforcing the downstreamslope. In a systematic risk analysis (see Section 6), not only the fail­ ure probability, but also the probable consequences of down­ streamdamage in case dambreach should occur, must be evalu­ ated. The extent of damage, particularly the potential loss of lives, depends entirely on the warning time available for the evacuation process. The warning time depends on the speed with which the failure (breaching) process andflood wave develop. Failure of a typical rockfill dam with anearth or asphalt core or an upstream facing, may be precipitated by one of several mechanisms, including: • Scour andunravelling of the downstreamtoe; • Scour andunravelling of the downstreamslope above the toe; • If the mechanisms above are prevented, failure by a more deep-seated sliding surface due to build-up of pore water pressures in the downstreamfill. If the rise of the reservoir is so rapid that not only the core is overtopped, but even the dam crest, other failure mechanisms may also develop (e.g. Leps, 1972; Parkin, 1991; Toledo, 1998). The overtopping may be caused by obstructed discharge facili­ ties during a flood or by sinkholes caused by severe piping due to internal leakage anderosion. Much research effort is now going into better defining the re­ quired drainage capacity, the resistance to overtopping, the breaching process andthe characteristics of the flood wave in the unlikely event that disaster strikes. Laboratory modelling tests, field tests and numerical simulations have been used in this ef­ fort (e.g. Fread, 1987; Yang, 1997; ICOLD, 1998). In Norway, for instance, a program is now underway (2001-2003) to study the behaviour of typical rockfill embankment dams under such extreme flow conditions. The program will include 6 m high field “model” embankments built specifically for this purpose, and brought to failure. The model dams are located immediately downstreamof anexisting dam, so the inflow may be accurately controlled by the gates. Rockfill dams built in Norway since 1980 have all been de­ signed with a special toe drain consisting of rocks larger than 0.5 m3 (see Fig. 5). When evaluating the drainage capacity of older dams, one must judge whether the rock size in the toe is sufficient to resist the rate of flow caused by a leakage incident of a specified low probability. The smallest stones in the toe will become unstable and unravel early in the process, but that may not have any effect on the overall stability of the load carrying skeleton of the toe. Reliable criteria do not exist for what grain size diameter to consider, e.g. d20 or dj0, and the effect of the shape of the grain size curve (i.e. uniformity coefficient). The planned research will address this and other issues, in order to derive criteria for strengthening existing toes and downstream slopes to resist accidental leakage andtemporary overtopping. 6 SYSTEMATIC RISKANALYSIS A useful definition of risk is the computed product of the prob­ ability of failure (or damage) and the expected cost (direct and indirect) of failure or damage, should it occur. However, fre­ quently in the literature and in the media one will also find that the wordrisk refers to probability of failure alone. When evaluating expected costs and consequences, one con­ siders potential downstreamdamage in terms of loss of life, inju­ ries, environmental and social effects, and material losses. There are special considerations for a cascade development along a river, andthe role of warning time achieved through surveillance and monitoring. The time delay in the dam-breach and flooding process may be crucial for the extent of the consequences, and appropriate preparedness and action plans may substantially de­ crease the computed risk (Lafitte, 1997; Funnemarket al„ 1998). The first papers on the potential usefulness of risk analysis in dam engineering appeared 25 years ago, and in other fields the methodology is being applied fairly extensively. There is now a renewed interest in probabilistic risk analysis for dams, and ICOLD is in the process of preparing “Guidelines on Risk As­ sessment for Dams". Kreuzer (2000) and Stewart (2000) recently presentedcomprehensive overviews. The main purpose of carrying out arisk analysis is to provide decision support. For many applications, the resulting numerical values do not have to be accurate in absolute terms, but must be inherently consistent so they allow reliable relative comparisons among alternatives. Going through such a systematic procedure gives insight which is an essential outcome in itself, and has di­ dactic value for owner, operator, consultant and safety profes­ sional. The procedure pinpoints specific features and conditions of the damandits operation where the largest riskreductions can be achieved. Risk analysis provides a framework for systematic appli­ cation of engineering judgement and available statistics in deci­ sion making. In this process it is common to use logic trees like event and/or fault trees. An event tree is constructed for each possible failure or damage mechanism. It is essential to decom­ pose each potential failure sequence into its components, thus defining branch points in the event tree. The better defined the mechanism and failure sequence, the easier it is to assign event probabilities, and the more reliable the failure probability esti­ mate. The probability estimates at each branch point in the tree may be determined fromacombination of: 2500
  • 12. • Statistical information relevant to the situation; • Probabilistic estimates obtained by introducing parameterun­ certainties in the deterministic model for the event consid­ ered, including information qn the dam’ s performance so far; and • Engineeringjudgement quantified by subjective probabilities. • The riskanalysis methodology maybe used: • At the dam design stage to ensure that the main efforts are placed where the uncertainties and theconsequences of unsat­ isfactory behaviour are the largest; • When re-evaluating safety of anexisting dam; • When selecting among different remedial actions for a par­ ticular dam and among dams in a cascade development (pri­ oritising); • When establishingemergency action plans andpreparedness; • To relate damengineering risk levels to acceptable (tolerable) risklevels established by society. The first four applications have proved to be very useful and are not controversial. The fifth application is very complex and the issue is sensitive as “acceptable risk” is not well defined. There will always have to be a trade-off between extra safety (reduced risk) and the increased use of society's resources. Inthe old days, engineers managed to agree on and get acceptance for using numerical values for safety factors. The public did not really know what they implied, but the factors gave a feeling of safety. We can no longer hide behind such deterministic factors without defining what they imply. Probabilistic risk analysis can assist us. However, to be accepted, the riskanalyses must be pre­ sented as credible, defensible, and transparent (e.g. Hartford, 1997). A reservation (or criticism) against probabilistic risk analysis is that one may overlook a future incident which would involve one or more failure mechanisms not included in the analysis. That is a most important concern and was referred to in Section 4. However, that concern is the same forour deterministic analy­ ses. Statistics show that it is the overlooking of aspects, not in­ adequate details of analyses, which cause unsatisfactory per­ formance andsometimes failure. The first step in aprobabilistic risk analysis is to carefully go through a "failure mode screening" where one visualises andde­ fines all potential failure modes. No probabilities are assigned at this stage, but some failure modes are eliminated by physical reasoning, and the arguments for elimination are recorded. Then anevent tree maybe constructed where the failure sequences are developed and detailed, displaying the interrelationships among events. The process may stop at this stage without providing quantitative probability estimates at each branch point in the event tree. A very systematic way of performing a failure mode screening is by means of the so-called failure modes and effects analysis (FMEA). This may be extended to a failure modes, ef­ fects and criticality analysis (FMECA) as described in BSI (1991) and applied by Beak et al„ (1997), Sandilands et al. (1998), andMcLeod andPlewes (1999). After several years of optimismin the profession with regard to developing and performing meaningful quantitative probabil­ istic risk analyses for dams and auxiliary structures, there now seems to be atrendtowards more use of the qualitative FMECA. However, with time there will be increasing pressure from the decision makers to quantify the risk level estimates so they may be compared with an "acceptable risk" or "public protection guidelines". In the Netherlands the development in this direction is quite advanced and used in the safety evaluation and upgrad­ ing of dikes and stormsurge barriers (Vrijling, 2001). 7 NEED FORDAMSAFETY LEGISLATIONAND DAM ENGINEERINGEDUCATION The approaches used to ensure dam safety in different regions and countries vary. For example, in Europe, more so than in North America, one is inclined to use safety legislation, codes and guidelines. Some of the reasons for the emphasis on this topic are (Hfleg, 1998): • Society today, more than arelatively few years ago, demands that safety evaluations be carried out and documented for ac­ tivities involving risks imposed on the public (as opposed to voluntary risks). Similar demands apply to certification and re-certification of nuclear power plants, chemical plants, off­ shore structures, bridges andinfrastructure in general. • More extensive records, and possibly changes in climatic conditions since the construction of a dam, necessitate updat­ ing of flood estimates and re-evaluation of dam safety. For instance, the flooding and dramatic failures in Saguenay in July 1996 have had important impacts on legislation and guidelines in Quebec, Canada. • Earthquake effects may have to be considered in regions ear­ lierclassified as non-seismic. • Significant changes in physical conditions both upstreamand downstream since the dam was built require a review of the risks involved andthe damsafety. • There are significant differences among damowners and op­ erators with respect to their qualifications and the rigour of their safety programmes, which must be updated to reflect: new information obtained from available data and statistics; improved understanding of failure and damage mechanisms; changes in general international safety standards; and the need for more objective approaches than were practised ear­ lier. • The recent deregulation of the energy market in many coun­ tries has resulted in changes in dam ownership, and placed more emphasis on required return on investment. One may therefore fear that alower priority may be placed on safety. • Environmental, social and dam safety considerations are closely interrelated. Hence, safety is brought into focus in the public debate, and more documentation is required relating to reliability and risklevels. • As stated in Section 5, ageing dams require continuous main­ tenance and rehabilitation, and strengthening may also be re­ quired. At the same time, and in many countries, the new generation of engineers responsible for this work receives very little hands-on experience with the design and construc­ tion of new dams, and relevant educational programmes in universities are gradually disappearing. Therefore, the use of dam safety legislation and fairly detailed requirements and guidelines are considered to be awayof ensuring safety. Regarding this last point it is interesting to note what Ter- zaghi said about education and practical experience in his Presi­ dential Address at the 4. ICSMFE (1957): “After the student has absorbed the theory of structures, soil mechanics andengineering geology with his head andhas passed the final examinations, his real development starts. The final outcome depends entirely on innate qualifications and environ­ ment. Many of those who have passed their examinations with flying colours are doomed to remain technicians to the end of their lives. They will never leam to walk without the crutches of step-for-step logical reasoning and no systemof education could change this condition. However, the same individual may turn into apoor technician or afirst-class one depending on the qual­ ity of the professional training he received, and that is important. Those few who were bomunder a luckier star mayrise gradually from the ranks of technicians to those of competent engineers, capable of thinking with both their heads andtheirhips. However, for given innate qualifications, the person with su­ perior training has atremendous advantage over the one who has received adeficient education. Therefore, engineering education should always be forus a matterof primaryconcern. Yet no mat­ terhow adequate the training may be, the prospects ofthe gradu­ ate to rise above the level of a technician are nil, irrespective of his innate qualifications, unless the following additional condi­ tion is satisfied. His subsequent professional activities must give him ample opportunity to compare his design assumptions and forecasts with the real conditions as disclosed by the subsequent 2501
  • 13. construction operations and the performance of the completed structures. Otherwise he lives, without knowing it, in afictitious world." Terzaghi searched for "men of judgement", to use his own phrase. In many parts of the world, e.g. Europe andNorth Amer­ ica, such damengineers will be hardto find, unless they get their experience fromcountries where dams are being built, or special field training programs are established. This is a challenge - the recruitment, education andpractical training of damengineers to take care of and upgrade where required, the aging dampopula­ tion. 7.1 Application o fnew criteria to old dams There is controversy about how new safety criteria shall be ap­ plied to existing structures, built under the regime of different criteria. In any such re-evaluation of an existing dam, due con­ sideration must be given to the dam's performance duringopera­ tion to date. With time, some of the uncertainties which had to be accounted for in the initial design and therefore may have re­ quired a higher design factor of safety (factor of uncertainty), have been erased. Statistically, most dam incidents and failures occur during first reservoir filling or shortly afterwards as the weaknesses in design and construction appear. As these uncer­ tainties no longer exist for astructure which has proved itself by performing well, the nominal (theoretically computed) safety factor does not have to be the same for an old and new dam. However, in principle, the computed probability of failure should not be allowed to be any higher for the old structure. (This is an illustration of the inadequacy of using the conven­ tional safety factor). The importance of past performance in the "re-certification” process points out the essential role of continuous monitoring. It enables the owner to document the dam's performance when the issue of satisfying newcriteriacomes up. A question which frequently arises for embankment dams is how to apply new and stricter filter criteria to an existing struc­ ture. Rather than requiring the replacement of interior filters, which may mean replacing the whole structure, the dam safety authorities should accept other measures to make sure that the overall dam safety level satisfies present standards. By that is meant that the risk imposed by the old structure should not be any higher than that for astructure satisfying the newfiltercrite­ ria. Othermeasures mayinclude: • Reducing flow velocity through the dam and thereby reduc­ ing the probability of initiating internal erosion (see Section 5.3); • Increasing downstream drainage capacity to handle a higher potential leakage (see Section 5.4); or • Improving monitoringof the dam. It is estimated that probability of failure in many cases may be reduced by an order of magnitude or more if proper moni­ toring is taking place, so that appropriate measures maybe taken in time. However, as stated by Leps (1988) about the rapid fail­ ure of the Teton Dam, even extensive instrumentation could probably not have provided any useful timely warning because there was no second line of defence (see Section4.1). 8 THEDEBATEABOUT DAMS AND SUSTAINABLE DEVELOPMENT It is not appropriate to finish this contribution on dam engi­ neering without referring to the intense debate that has been tak­ ing place in recent years - and which will go on. At the time Terzaghi worked with dams for development projects around the world, there was little concern about the disbenefits dams may create. The benefits were considered so overpowering to the country andregion at large, that anyrequireddisplacement of lo­ cal people and any negative local ecological effects were "ac­ cepted". That is no longer the case as rigorous studies are re­ quired, and all options considered, before it is decided that dam building is the best alternative to satisfy the needs in question. Table 6 shows the different functions of the world’s large dams (ICOLD, 1998). Very many dams are multi-purpose serv­ ing more thanone function. Proponents maintain that dams have generally performed very well as an integral part of water and energy resource development strategies in over 140 nations and, with some exceptions, have provided an indispensable range of water and energy services. Opponents contend that better, cheaper and more benign options exist and have frequently been ignored. Table 6. Functions of the world's large dams Irrigation 48% Electricity generation 20% Water supply 15% Flood protection/control 8% Recreation and improved environment 4% Inland navigation 2% Fish breeding 2% Fire fighting and miscellaneous 1% ICOLD (1997) has set down its guidelines, and a recent exten­ sive study initiated by the World Bank and the World Conserva­ tion Union, concludes that (WCD, 2000): • Dams have made animportant and significant contribution to humandevelopment, and the benefits derived fromthemhave been considerable. • In many cases an unacceptable and often unnecessary price has been paid to secure those benefits, especially in social and environmental terms, by people displaced, by communities downstream, by taxpayers andby the natural environment. • Lack of equity in the distribution of benefits has called into question the value of many dams in meeting waterandenergy development needs when compared with the alternatives. • By bringing to the table all those whose rights are involved and who bear the risks associated with different options for water and energy resources development, the conditions for a positive resolution of competing interests and conflicts are created. • Negotiating outcomes will greatly improve the development effectiveness of water and energy projects by eliminating un­ favourable projects at an early stage, and by offering as a choice only those options that key stakeholders agree repre­ sent the best ones to meet the needs in question. Looking ahead, people will continue to build dams for many purposes, especially in the developing world. The reason is that dams in very many cases will bejudged to represent the best op­ tion among the feasible alternatives to satisfy critical human and societal needs. However, a more systematic procedure of option assessment should be developed and practised, to facilitate the decision making. As the world population continues to increase in water-scarce regions and concentrate in mega-cities, additional water re­ sources must be developed. The only practical way to achieve this on the scale required is to increase storage capacity. With our increased knowledge and understanding, the dams will be made socially equitable and environmentally sustainable through stakeholder involvement, monitoring and continuous evaluation. REFERENCES ASCE (1998) Report Card for America's Infrastructure, in Issue Brief- Dams, American Society of Civil Engineers, 5 March 1998. 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