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International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072
© 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5348
Literature Review on Liquefaction Screening using CPT
Reza, Md. Selim1, Rana, Md. Sohel2
1Senior Lecturer, Uttara University, Uttara, Dhaka, Bangladesh
2Assistant Engineer, Local Government Engineering Department (LGED), Dhaka, Bangladesh
---------------------------------------------------------------------***----------------------------------------------------------------------
Abstract - Assessing liquefaction screening and potential
for clean sands and silty sands remains a difficult problem:
how the fines content affects the cyclic resistance ratio (CRR),
consolidation characteristics, and cone resistance in CPT still
not clearly understood. To assess liquefaction potential,
liquefaction screening charts depicting a correlation between
cyclic resistance ratio (CRR) and normalized cone resistance
(qc1N) has been evolved based upon past earthquake case
histories and laboratory study. Whether a site would be
liquefiable or non-liquefiable can be crudely evaluated by the
demarcation line indicating the relationshipbetweenCRR and
qc1N. It has been observed that the demarcation line shifting
towards left with the increases of silty content: sands and silty
sands with the same cone resistance can have different
liquefaction resistance. In field observation, the difficulty in
assessing the in-situ condition during earthquake leads the
researchers to assess the liquefaction potential of
corresponding soil in laboratory study. In this paper, how the
silt content alters the intergrain contact density, affect the
cyclic resistance, consolidation characteristics have been
presented. The reduction in cone resistance, shifting the CRR-
qc1N curves towards left as silt content increases, canbeclearly
understood by coefficient of consolidation rather than gross
silt content. In laboratory CPT, the effect of silt content on
normalized cone resistance (qc1N) has been observed through
intergrain contact density and consolidation characteristics.
Normalized penetration rate, To (=v*dc/cv, where visthecone
penetration rate, dc is the cone diameter of the cone and cv is
the coefficient of consolidation) has been introduced into the
CRR-qc1N charts and compared with the current liquefaction
screening charts based onCRR-qc1N-FC, whereFCisthepercent
silt content.
Key Words: Liquefaction, Cone resistance, Silt content,
density, consolidation, permeability
1. INTRODUCTION
The term liquefaction has been used in concurrence with a
variety of phenomena thatincludessoil deformationscaused
by disturbance from monotonic, transient, or repeated
loading of saturated cohesionless soils under partially
undrained or undrained conditions. Developing excess pore
water pressure and dissipation of the pressure is the main
factor in all liquefaction phenomena. As shown in the figure
below, when a soil is experiencing effective stress large
enough to cause slip among grain contacts, the contacts
between soil particles become instable and transfer the
forces carried by contacts to water hence develop the pore
water pressure.
1.1 Liquefaction phenomena
Liquefaction phenomena could be divided into two
main categories: flow liquefaction and cyclic softening.Flow
liquefaction can happen when the shear stress necessaryfor
static equilibrium of a soil mass is greater than the shear
strength of the soil in its liquefied state [6],[7]. In contrast to
flow liquefaction, cyclic mobility occurs when the static
shear stress is less than the shear strength of the liquefied
soil. There have been many studies focused on identifying
the factors and mechanisms causing liquefaction [5], [13],
[17]. Size, shape, and gradation spectrum of soil particles,
initial relative density, fines content, stress level, drainage
characteristics, previous strain history, vibration
characteristics, period of loading, and tapped air are the
main factors affect the liquefaction process
2. Literature review
Liquefaction screening techniques, empirical relation
between liquefaction resistanceandfielddata evolved based
upon knowledge from laboratory research conducted on
clean sands and observed field performance during past
earthquakes [24], are to measure the liquefaction potential
of a site. To evaluate the soil in liquefaction resistance
capacity, researcher began to study previous case history of
sites: liquefied and non-liquefiedduringearthquake.Thesoil
resistance is measured in the study site by the availablefield
test like Standard Penetration Test (SPT), Cone Penetration
Test (CPT) and Shear Wave velocity (Vs). Fig-1 presents the
liquefaction resistance, cyclic stress ratio (CSR) and soil
resistance (N1)60 of different sites. Demarcation line have
been drawn between liquefied and non-liquefied sites.
Current liquefaction screening of clean sandsandsiltysands
from in-situ tests results, standard penetration test (SPT),
cone penetration test (CPT) and shear wave velocity, have
been correlated to cyclic resistance ratio (CRR) for different
fines content [1], [11], [10], [14], [16]. Field observation of
liquefaction screening provides the clean sand base curve
and suggest an extrapolation to account fines content in
soils. However, how the fines affecttheliquefactionpotential
assessment is not clearly understood which leads to
researcher to explore silt-phenomenon in the liquefaction
screening chart.
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072
© 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5349
Fig-1: Cyclic Stress Ratio vs Soil Resistance [4], [10]
It has been observed from the Fig-1, at the same penetration
resistance, (N1)60, soil has different liquefaction resistance
which leads the researcher to study the factors causing
liquefaction other than density. The ability of continuous
recording of soil profile, conepenetrationtest(CPT)hasbeen
utilized to brand the liquefaction potential ofsoilsbyrelating
the normalized cone tip resistance-qc1N to the cyclic
resistance ratio (CRR) – Fig-2.
Fig-2: Cyclic Resistance Ratio (CRR) vs CPT tip resistance
[11]
2.1. Liquefaction screening for sands and silty
sands using CPT
SPT, CPT and shear wave velocity are the means of current
approaches to evaluate potential liquefaction. Among, CPT
has gained attention to the researcher because of its
continuous profiling ofsoil strata withoutmissingthinlayers
and repeatability of the test. [10], [14] converted SPT based
potential liquefaction assessment data to equivalent CPT
based assessment to evaluate the liquefaction potential as
presented in Fig-3.
Fig-3: Liquefaction potential evaluation charts using CPT
[10], [14]
It is observed in Fig.-3 that coarsersoilhaslowerliquefaction
resistance than the finer one. And also showed that sands
with fines has more resistance against liquefaction at the
same resistance than the clean sands [14].
0
0.1
0.2
0.3
0.4
0.5
0.6
0 50 100 150 200 250
(CRR)field-ave
qc1N
Idriss and Boulanger, 2014
FC=5%
15%
30%70%
Fig-4: Liquefaction evaluation charts using CPT [4]
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072
© 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5350
Fig-4. presents thecorrelationbetweenconeresistance(qc1N)
and CRR at earthquake magnitude 7.5. It is noticed that the
(CRR)7.5-qc1N curves shifting towards left as silts content
increases indicating that the clean sand has less liquefaction
resistance than the sands with silt. It is also noticed that the
liquefaction demarcation lineevolvingthroughexperienceof
researcher and practioners. It is also can be concluded from
Fig-4 that the silts has little prone toliquefactionasthe100%
curve would be almost vertical: Implied from the trend of
shifting the curve to the left as fines content increases. And
the normalized cone resistance (qc1N) is calculated as:
qc1N = = CQ (Eqn. 1)
Where qc is the field cone resistance and Pa is the
atmospheric pressure.
And CQ is the overburden correction factor defined by [16],
CQ = (Eqn. 2)
Where σ’vo is the effective overburden pressure and Pat is
the atmospheric pressure.
Or By [24]
CQ = ≤ 1.7 (Eqn. 3)
Where stress exponent (n) varies fromaround0.5insandsto
1.0 in clays. For sands and silty sands 0.5consideredforthen
value.
2.2 Liquefaction Screening Based upon Laboratory
Study
To understand the characteristics of liquefaction in silty
sands, researchers began to investigate the effect of fines on
liquefaction resistance[22].Itisreportedthatthemechanical
behaviors of clean sand and silty sand are very similar at a
given ‘equivalent’ inter-granular relative density (Drc)eq [23].
The effect of fines content is reflectedbypermeability(k)and
coefficient ofconsolidation(Cv)insaturatedsand-siltmixture
[15], [21]. Along with the soil properties (k, Cv), non-soil
parameters such as penetration rate of the cone, and
diameter of the cone have influence in the reduction of cone
resistance in saturated silty sands. Normalized penetration
rate T0 (T0=v*dc/cv, where v is the penetration velocity, dc is
the diameter of cone) incorporated the three factors causing
the reduction in saturated test [9]. Huang (2014) designed a
new chamber testing, capable of simulating the condition of
constant vertical stress and zero lateral strain (ideally)-BC3.
Conduct CPTs using Ottawa F55 saturated sand-silt mix at
different fines contents (0,15and 25%) to examine the effect
of fines on the cone resistance at differentfinescontent(0,15
and 25%) [3]. In continuation of Huang (2014) study,
Sivaratnarajah (2016) conducted several test at dry and
saturated conditiononsand-siltmixturetoexaminetheeffect
of To on the cone resistance and justify the findings of Huang
2014 study [12].
2.2.1 Contact Density Index-A Framework to
Intergranular Void Ratio
As stated earlier that sands with silts has different
characteristic than the clean sands. At the same global void
ratio (e) silty sand have different mechanical properties
compared with the clean sands because global void ratio
indicates only the voids in the sample but does not give how
fines oriented in the voids of the coarser grains and how it
affects the force chain in thesoilmatrix.Earlierstudyshowed
that the global void is a poor index of soil mixtures. This
problem leadsresearchertodeveloptheequivalentvoidratio
concept [17], [23] which proposes that the mechanical
properties such as steady state strength, liquefaction
resistance (CRR),stress-straincharacteristicsareexpectedto
be same for both clean sand and silty sand at the same
contact density index. To address this effect, [20], [23]
developed a soil matrix classification system.
2.2.2 Normalized Penetration Rate
As stated earlier, the evaluation process of liquefaction
potential based upon qC1N – CRRcurvedoesnotgiveanyclear
idea how finesaffect the coneresistance. The essenceoffines
in the liquefaction resistance leads further research on the
effect of fines content in the difference in cone resistance for
silty sands and other soil mixtures. The difference in cone
resistance results from thevariousdrainageconditionswhen
the cone advances into different soils: for example, the clean
sand undergoes drained condition asithashighpermeability
and the excess pore water pressure dissipates fast thus no
significant reduction. As the penetration rate (v) and the
diameter of the cone (dc) also contribute to the cone
resistance a non-dimensional penetration rate To [9] is
introduce to show the combined effect of degree of
consolidation during penetration as below:
To = (Eqn. 4)
Where,
To= Normalized penetration rate
V= velocity of cone
dc = diameter of cone
cv = coefficient of consolidation
2.2.3 Cyclic Stress Ratio (CSR)
According to [13], the cyclic stress ratio, CSR, as the average
cyclicshear stress, 𝜏 𝑎𝑣, developed on thehorizontalsurfaceof
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072
© 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5351
soil layers due to vertically propagating shear waves
normalized by the initial vertical effective stress, 𝜎 𝑣′, to
include the increase in shear strength due to increase in
effective stress. By accordingly weighting the individual
stress cycles based on laboratory test data, it has been found
that a rational amplitude to use for the “average” or
equivalent uniform stress, 𝜏𝑎𝑣, isabout65%ofthemaximum
shear stress.
𝐶𝑆𝑅= = 0.65( ) ( ) rd……. (Eqn.5)
where
𝑎 𝑚𝑎𝑥 = maximum horizontal ground surface acceleration (g)
𝑔 = gravitational acceleration
𝜎 𝑣 = total overburden pressure at depth z
𝜎 𝑣′ = effective overburden pressure at depth z
𝑟 𝑑 = stress reduction factor
The stress reduction factor, rd, is used to determine the
maximum shear stress at different depths in the soil. As
shown in the Fig-5 rd, values generally range from 1 at the
ground surface to lower values at larger depths.
Fig-5: Reduction factor to estimate the variation of cyclic
shear stress with depth below level or gently sloping
ground surface [24]
2.2.4 Cyclic Resistance Ratio (CRR)
The cyclic resistance ratio (CRR) represents the maximum
cyclic stress ratio (CSR) at which a given soil can resist the
liquefaction. In summary, CRR is the capacity of the soil
against liquefaction and CSR is the field stress induced by
shear loading.
Factor of safety against liquefaction,
FSL = (MSF* CRR7.5)/ (CSR) ……… (Eqn. 6)
Where MSF is the magnitude scaling factor, CRR7.5 is the
cyclic resistance ration at earthquake magnitude 7.5.
Fig-6 shows comparison between in-situ evolved CRR-qc1N
and laboratory calculated CRR from laboratory CPT. The
effect normalized penetration rate, To on the CRR and qc1N
has been observed from the figure. The prime limitation for
this comparison of CRR fromlaboratorystudyandin-situtest
is the equivalent conversion factors like earth pressure
coefficient, Ko. The earth pressure coefficient is dependent
upon the stress history, soil age, and relativedensityofsoil.It
is difficult to determine the in-situ earth pressure coefficient
hence the converted CRR might not give exact in-situ field
condition. The cyclic resistance ratio from triaxial test,
(CRR)tx is presumed to be the function of relative density
only, which is questionable because the liquefaction
resistance is depend on many other factors, like silt content,
drainage condition.
Fig-6: Comparison of laboratory (CRR) to field computed
CRR [12]
3. CONCLUSIONS
The current liquefaction screening technique by using CPT
primarily rely on knowledgefromextensivelaboratorystudy
conducted on clean sands and extrapolationofobservedfield
performance of past earthquake. It has been observed that
the demarcation line delineating liquefiable and non-
liquefiable soil shifting towards left as silt content increases
inliquefactionscreeningcharts:liquefactionresistance(CRR)
increases with the increases of silt content in soil at the same
cone resistance (qc1N). There is no clear consensus how the
silt contentaffectstheliquefactionresistanceandpenetration
resistance which leads the researcher to investigate the silt-
phenomena.
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072
© 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5352
Based upon the literature review, the effect of silt content in
the liquefaction screening technique can be summarized
through the following manners:
i) Silt particles in silty sands partially contribute to
cyclic resistance ratio CRR and cone resistance
qc1N in contrast to its full contribution to the
density: liquefaction resistance and cone
resistance of silty sands may not be as high as
that of clean sands.
ii) Silts content, reduces the pore size and the
permeability, inhibits the dissipation of
developed excess pore pressure around the
cone which leadsa reduction in coneresistance.
iii) Normalized cone penetration rate, To have been
introduced gross fines content in liquefaction
screening chart to incorporate coefficient of
consolidationandnon-soilpropertylikevelocity
of cone penetration and diameter of the cone in
the liquefaction screening chart. It is highly
likely that there exist a relationship between
CRR-qc1N-To.
ACKNOWLEDGEMENT
The authors acknowledge the helps from Professor Dr.
Sabanayagam Thevanayagam, Professor, University at
Buffalo, The state university of New York, USA.
REFERENCES
[1] Andrus, R. D. and Stokoe, K. H. ,2000. "Liquefaction
resistance of soils from shearwave velocity", J. Geotech.
and Geoenv. Eng., ASCE, Vol. 126(11), 1015-1025
[2] Boulanger, R. W., and Idriss, I. M., 2014. “CPT and SPT
based liquefaction triggering procedures.” Report No.
UCD/CGM-14/01, Center for Geotechnical Modeling,
Department of Civil and Environmental Engineering,
University of California, Davis, CA, 134 pp.
[3] Huang Q. 2014 Effect of nonplastic fines on cone
resistance in silty sand, PhD Dissertation, University at
Buffalo, Buffalo, NY.
[4] Idriss, I. M. and Boulanger, R. W., 2008. "Soil liquefaction
during earthquakes", Monograph MNO-12, Earthquake
Engineering Research Institute, Oakland, CA, 261 pp.
[5] Ishihara, K. (1993) “Liquefaction and flowfailureduring
earthquakes” Geotechnique, Vol. 43(3), 351-441
[6] Kramer, S. L. and Seed, H. B. (1988) “Initiation of soil
liquefaction under static loading conditions” J. of
Geotech. Eng., ASCE, Vol. 114(4), 412-430
[7] Kramer, S. L. (1996), Geotechnical Earthquake
Engineering, Prentice-Hall, Englewood Cliffs, NJ, 653p.
[9] Randolph, M. F. and Hope, S., 2004. "Effect of cone
velocity on the cone resistance and excess pore
pressures", IS Osaka - Engineering Practice and
Performance of Soft Deposits, Osaka, Japan, 147-152.
[10] Robertson, P. K. and Campanella, R. G. (1985)
“Liquefaction potential of sands using the CPT” Journal
of Geotechnical Eng., Vol. 111(3), 384-403
[11] Robertson, P. K., and Wride (Fear), C. E.,1998.
"Evaluating cyclic liquefaction potential using the cone
penetration test", Canadian Geotechnical Journal, 35,
442–459.
[12] Sivaratnarajah, U. 2016, Effect of non-plastic silt on
cone resistance, MS Dissertation, University at Buffalo,
Buffalo, NY,.
[13] Seed H. B., Idriss, I. M., and Arango I.(1983).“Evaluation
of liquefaction potential using fieldperformancedata.”J.
Geotech. Eng., ASCE, 109(3): 458-482.
[14] Seed, H. B., and De Alba, P. ,1986. "Use of SPT and CPT
tests for evaluating the liquefactionresistanceofsands.’’
Proceeding, Speciality Conference on Use of In-Situ
Testing in 88
[15] Shenthan, T. ,2001. "Factors affecting liquefaction
mitigation in silty soils using stone columns", M.S.
Thesis, State University of New York at Buffalo, NY.
[16] Stark, T. D., and Olson, S. M., 1995. "Liquefaction
resistance using CPT and field case histories.’’ Journal of
Geotechnical Engineering, 121(12), 856–869.
[17] Thevanayagam, S. (2000a) “Liquefaction potential and
undrained fragility of silty soils” Proc. of the 12th Int.
World Conf. on Earthquake Engineering, Auckland,New
Zealand, 124-131
[18] Thevanayagam, S. (2000b) “Liquefaction in silty soils -
Considerations forscreening andretrofitstrategies”2nd
Workshop on Mitigation of Seismic Effects on
Transportation Structures, Taipei, Taiwan
[19] Thevanayagam, S. and Mohan,S.(2000a)“Intergranular
state variables and stress-strain behavior of silty soils”
Geotechnique, Vol. 50(1), 1-23
[20] Thevanayagam, S., Liang, J. and Shenthan, T. (2000b)
“Contact index andliquefactionpotential analysisofsilty
and gravely soils” Proc. 14th ASCE Engineering
Mechanics Conference, Austin, TX.
[21] Thevanayagam, S. and Martin, G. R. 2002. "Liquefaction
in silty soils – screening and remediation issues ", Soil
Dynamics and Earthquake Engineering, Vol. 22, 1035-
1042.
[22] Thevanayagam, S., Shenthan, T., and Kanagalingam, T.,
(2003). Role of intergranular contacts on mechanisms
causing liquefaction and slope failures in silty sands.
Final Report, USGS Award No. 01HQGR0032 and
99HQGR0021; US Geological Survey, Department of
Interior, USA, 396p.
[23] Thevanayagam, S., Shenthan, T., Mohan, S., and Liang, J.,
2002. "Undrained fragilityof cleansands,siltysandsand
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056
Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072
© 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5353
sandy silts", Journal of Geotechnical and
Geoenvironmental Engineering, 128(10),849-859.
[24]Youd, T.L., and Idriss, I.,M., 2001. "Liquefaction
resistance of soils: summary report from 1996 NCEER
and 1998 NCEER/NSF workshops on evaluation of
liquefaction resistance of soils", Journal of Geotechnical
and Geoenvironmental Engineering, 127(4), 297-31.
BIOGRAPHIES
Md. Selim Reza
M.Sc. (University at Buffalo)
Senior Lecturer, Uttara University
Dhaka, Bangladesh
Md. Sohel Rana
B.Sc. (DUET, Bangladesh)
Assistant Engineer, LGED,
Bangladesh

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IRJET- Literature Review on Liquefaction Screening using CPT

  • 1. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072 © 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5348 Literature Review on Liquefaction Screening using CPT Reza, Md. Selim1, Rana, Md. Sohel2 1Senior Lecturer, Uttara University, Uttara, Dhaka, Bangladesh 2Assistant Engineer, Local Government Engineering Department (LGED), Dhaka, Bangladesh ---------------------------------------------------------------------***---------------------------------------------------------------------- Abstract - Assessing liquefaction screening and potential for clean sands and silty sands remains a difficult problem: how the fines content affects the cyclic resistance ratio (CRR), consolidation characteristics, and cone resistance in CPT still not clearly understood. To assess liquefaction potential, liquefaction screening charts depicting a correlation between cyclic resistance ratio (CRR) and normalized cone resistance (qc1N) has been evolved based upon past earthquake case histories and laboratory study. Whether a site would be liquefiable or non-liquefiable can be crudely evaluated by the demarcation line indicating the relationshipbetweenCRR and qc1N. It has been observed that the demarcation line shifting towards left with the increases of silty content: sands and silty sands with the same cone resistance can have different liquefaction resistance. In field observation, the difficulty in assessing the in-situ condition during earthquake leads the researchers to assess the liquefaction potential of corresponding soil in laboratory study. In this paper, how the silt content alters the intergrain contact density, affect the cyclic resistance, consolidation characteristics have been presented. The reduction in cone resistance, shifting the CRR- qc1N curves towards left as silt content increases, canbeclearly understood by coefficient of consolidation rather than gross silt content. In laboratory CPT, the effect of silt content on normalized cone resistance (qc1N) has been observed through intergrain contact density and consolidation characteristics. Normalized penetration rate, To (=v*dc/cv, where visthecone penetration rate, dc is the cone diameter of the cone and cv is the coefficient of consolidation) has been introduced into the CRR-qc1N charts and compared with the current liquefaction screening charts based onCRR-qc1N-FC, whereFCisthepercent silt content. Key Words: Liquefaction, Cone resistance, Silt content, density, consolidation, permeability 1. INTRODUCTION The term liquefaction has been used in concurrence with a variety of phenomena thatincludessoil deformationscaused by disturbance from monotonic, transient, or repeated loading of saturated cohesionless soils under partially undrained or undrained conditions. Developing excess pore water pressure and dissipation of the pressure is the main factor in all liquefaction phenomena. As shown in the figure below, when a soil is experiencing effective stress large enough to cause slip among grain contacts, the contacts between soil particles become instable and transfer the forces carried by contacts to water hence develop the pore water pressure. 1.1 Liquefaction phenomena Liquefaction phenomena could be divided into two main categories: flow liquefaction and cyclic softening.Flow liquefaction can happen when the shear stress necessaryfor static equilibrium of a soil mass is greater than the shear strength of the soil in its liquefied state [6],[7]. In contrast to flow liquefaction, cyclic mobility occurs when the static shear stress is less than the shear strength of the liquefied soil. There have been many studies focused on identifying the factors and mechanisms causing liquefaction [5], [13], [17]. Size, shape, and gradation spectrum of soil particles, initial relative density, fines content, stress level, drainage characteristics, previous strain history, vibration characteristics, period of loading, and tapped air are the main factors affect the liquefaction process 2. Literature review Liquefaction screening techniques, empirical relation between liquefaction resistanceandfielddata evolved based upon knowledge from laboratory research conducted on clean sands and observed field performance during past earthquakes [24], are to measure the liquefaction potential of a site. To evaluate the soil in liquefaction resistance capacity, researcher began to study previous case history of sites: liquefied and non-liquefiedduringearthquake.Thesoil resistance is measured in the study site by the availablefield test like Standard Penetration Test (SPT), Cone Penetration Test (CPT) and Shear Wave velocity (Vs). Fig-1 presents the liquefaction resistance, cyclic stress ratio (CSR) and soil resistance (N1)60 of different sites. Demarcation line have been drawn between liquefied and non-liquefied sites. Current liquefaction screening of clean sandsandsiltysands from in-situ tests results, standard penetration test (SPT), cone penetration test (CPT) and shear wave velocity, have been correlated to cyclic resistance ratio (CRR) for different fines content [1], [11], [10], [14], [16]. Field observation of liquefaction screening provides the clean sand base curve and suggest an extrapolation to account fines content in soils. However, how the fines affecttheliquefactionpotential assessment is not clearly understood which leads to researcher to explore silt-phenomenon in the liquefaction screening chart.
  • 2. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072 © 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5349 Fig-1: Cyclic Stress Ratio vs Soil Resistance [4], [10] It has been observed from the Fig-1, at the same penetration resistance, (N1)60, soil has different liquefaction resistance which leads the researcher to study the factors causing liquefaction other than density. The ability of continuous recording of soil profile, conepenetrationtest(CPT)hasbeen utilized to brand the liquefaction potential ofsoilsbyrelating the normalized cone tip resistance-qc1N to the cyclic resistance ratio (CRR) – Fig-2. Fig-2: Cyclic Resistance Ratio (CRR) vs CPT tip resistance [11] 2.1. Liquefaction screening for sands and silty sands using CPT SPT, CPT and shear wave velocity are the means of current approaches to evaluate potential liquefaction. Among, CPT has gained attention to the researcher because of its continuous profiling ofsoil strata withoutmissingthinlayers and repeatability of the test. [10], [14] converted SPT based potential liquefaction assessment data to equivalent CPT based assessment to evaluate the liquefaction potential as presented in Fig-3. Fig-3: Liquefaction potential evaluation charts using CPT [10], [14] It is observed in Fig.-3 that coarsersoilhaslowerliquefaction resistance than the finer one. And also showed that sands with fines has more resistance against liquefaction at the same resistance than the clean sands [14]. 0 0.1 0.2 0.3 0.4 0.5 0.6 0 50 100 150 200 250 (CRR)field-ave qc1N Idriss and Boulanger, 2014 FC=5% 15% 30%70% Fig-4: Liquefaction evaluation charts using CPT [4]
  • 3. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072 © 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5350 Fig-4. presents thecorrelationbetweenconeresistance(qc1N) and CRR at earthquake magnitude 7.5. It is noticed that the (CRR)7.5-qc1N curves shifting towards left as silts content increases indicating that the clean sand has less liquefaction resistance than the sands with silt. It is also noticed that the liquefaction demarcation lineevolvingthroughexperienceof researcher and practioners. It is also can be concluded from Fig-4 that the silts has little prone toliquefactionasthe100% curve would be almost vertical: Implied from the trend of shifting the curve to the left as fines content increases. And the normalized cone resistance (qc1N) is calculated as: qc1N = = CQ (Eqn. 1) Where qc is the field cone resistance and Pa is the atmospheric pressure. And CQ is the overburden correction factor defined by [16], CQ = (Eqn. 2) Where σ’vo is the effective overburden pressure and Pat is the atmospheric pressure. Or By [24] CQ = ≤ 1.7 (Eqn. 3) Where stress exponent (n) varies fromaround0.5insandsto 1.0 in clays. For sands and silty sands 0.5consideredforthen value. 2.2 Liquefaction Screening Based upon Laboratory Study To understand the characteristics of liquefaction in silty sands, researchers began to investigate the effect of fines on liquefaction resistance[22].Itisreportedthatthemechanical behaviors of clean sand and silty sand are very similar at a given ‘equivalent’ inter-granular relative density (Drc)eq [23]. The effect of fines content is reflectedbypermeability(k)and coefficient ofconsolidation(Cv)insaturatedsand-siltmixture [15], [21]. Along with the soil properties (k, Cv), non-soil parameters such as penetration rate of the cone, and diameter of the cone have influence in the reduction of cone resistance in saturated silty sands. Normalized penetration rate T0 (T0=v*dc/cv, where v is the penetration velocity, dc is the diameter of cone) incorporated the three factors causing the reduction in saturated test [9]. Huang (2014) designed a new chamber testing, capable of simulating the condition of constant vertical stress and zero lateral strain (ideally)-BC3. Conduct CPTs using Ottawa F55 saturated sand-silt mix at different fines contents (0,15and 25%) to examine the effect of fines on the cone resistance at differentfinescontent(0,15 and 25%) [3]. In continuation of Huang (2014) study, Sivaratnarajah (2016) conducted several test at dry and saturated conditiononsand-siltmixturetoexaminetheeffect of To on the cone resistance and justify the findings of Huang 2014 study [12]. 2.2.1 Contact Density Index-A Framework to Intergranular Void Ratio As stated earlier that sands with silts has different characteristic than the clean sands. At the same global void ratio (e) silty sand have different mechanical properties compared with the clean sands because global void ratio indicates only the voids in the sample but does not give how fines oriented in the voids of the coarser grains and how it affects the force chain in thesoilmatrix.Earlierstudyshowed that the global void is a poor index of soil mixtures. This problem leadsresearchertodeveloptheequivalentvoidratio concept [17], [23] which proposes that the mechanical properties such as steady state strength, liquefaction resistance (CRR),stress-straincharacteristicsareexpectedto be same for both clean sand and silty sand at the same contact density index. To address this effect, [20], [23] developed a soil matrix classification system. 2.2.2 Normalized Penetration Rate As stated earlier, the evaluation process of liquefaction potential based upon qC1N – CRRcurvedoesnotgiveanyclear idea how finesaffect the coneresistance. The essenceoffines in the liquefaction resistance leads further research on the effect of fines content in the difference in cone resistance for silty sands and other soil mixtures. The difference in cone resistance results from thevariousdrainageconditionswhen the cone advances into different soils: for example, the clean sand undergoes drained condition asithashighpermeability and the excess pore water pressure dissipates fast thus no significant reduction. As the penetration rate (v) and the diameter of the cone (dc) also contribute to the cone resistance a non-dimensional penetration rate To [9] is introduce to show the combined effect of degree of consolidation during penetration as below: To = (Eqn. 4) Where, To= Normalized penetration rate V= velocity of cone dc = diameter of cone cv = coefficient of consolidation 2.2.3 Cyclic Stress Ratio (CSR) According to [13], the cyclic stress ratio, CSR, as the average cyclicshear stress, 𝜏 𝑎𝑣, developed on thehorizontalsurfaceof
  • 4. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072 © 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5351 soil layers due to vertically propagating shear waves normalized by the initial vertical effective stress, 𝜎 𝑣′, to include the increase in shear strength due to increase in effective stress. By accordingly weighting the individual stress cycles based on laboratory test data, it has been found that a rational amplitude to use for the “average” or equivalent uniform stress, 𝜏𝑎𝑣, isabout65%ofthemaximum shear stress. 𝐶𝑆𝑅= = 0.65( ) ( ) rd……. (Eqn.5) where 𝑎 𝑚𝑎𝑥 = maximum horizontal ground surface acceleration (g) 𝑔 = gravitational acceleration 𝜎 𝑣 = total overburden pressure at depth z 𝜎 𝑣′ = effective overburden pressure at depth z 𝑟 𝑑 = stress reduction factor The stress reduction factor, rd, is used to determine the maximum shear stress at different depths in the soil. As shown in the Fig-5 rd, values generally range from 1 at the ground surface to lower values at larger depths. Fig-5: Reduction factor to estimate the variation of cyclic shear stress with depth below level or gently sloping ground surface [24] 2.2.4 Cyclic Resistance Ratio (CRR) The cyclic resistance ratio (CRR) represents the maximum cyclic stress ratio (CSR) at which a given soil can resist the liquefaction. In summary, CRR is the capacity of the soil against liquefaction and CSR is the field stress induced by shear loading. Factor of safety against liquefaction, FSL = (MSF* CRR7.5)/ (CSR) ……… (Eqn. 6) Where MSF is the magnitude scaling factor, CRR7.5 is the cyclic resistance ration at earthquake magnitude 7.5. Fig-6 shows comparison between in-situ evolved CRR-qc1N and laboratory calculated CRR from laboratory CPT. The effect normalized penetration rate, To on the CRR and qc1N has been observed from the figure. The prime limitation for this comparison of CRR fromlaboratorystudyandin-situtest is the equivalent conversion factors like earth pressure coefficient, Ko. The earth pressure coefficient is dependent upon the stress history, soil age, and relativedensityofsoil.It is difficult to determine the in-situ earth pressure coefficient hence the converted CRR might not give exact in-situ field condition. The cyclic resistance ratio from triaxial test, (CRR)tx is presumed to be the function of relative density only, which is questionable because the liquefaction resistance is depend on many other factors, like silt content, drainage condition. Fig-6: Comparison of laboratory (CRR) to field computed CRR [12] 3. CONCLUSIONS The current liquefaction screening technique by using CPT primarily rely on knowledgefromextensivelaboratorystudy conducted on clean sands and extrapolationofobservedfield performance of past earthquake. It has been observed that the demarcation line delineating liquefiable and non- liquefiable soil shifting towards left as silt content increases inliquefactionscreeningcharts:liquefactionresistance(CRR) increases with the increases of silt content in soil at the same cone resistance (qc1N). There is no clear consensus how the silt contentaffectstheliquefactionresistanceandpenetration resistance which leads the researcher to investigate the silt- phenomena.
  • 5. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072 © 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5352 Based upon the literature review, the effect of silt content in the liquefaction screening technique can be summarized through the following manners: i) Silt particles in silty sands partially contribute to cyclic resistance ratio CRR and cone resistance qc1N in contrast to its full contribution to the density: liquefaction resistance and cone resistance of silty sands may not be as high as that of clean sands. ii) Silts content, reduces the pore size and the permeability, inhibits the dissipation of developed excess pore pressure around the cone which leadsa reduction in coneresistance. iii) Normalized cone penetration rate, To have been introduced gross fines content in liquefaction screening chart to incorporate coefficient of consolidationandnon-soilpropertylikevelocity of cone penetration and diameter of the cone in the liquefaction screening chart. It is highly likely that there exist a relationship between CRR-qc1N-To. ACKNOWLEDGEMENT The authors acknowledge the helps from Professor Dr. Sabanayagam Thevanayagam, Professor, University at Buffalo, The state university of New York, USA. REFERENCES [1] Andrus, R. D. and Stokoe, K. H. ,2000. "Liquefaction resistance of soils from shearwave velocity", J. Geotech. and Geoenv. Eng., ASCE, Vol. 126(11), 1015-1025 [2] Boulanger, R. W., and Idriss, I. M., 2014. “CPT and SPT based liquefaction triggering procedures.” Report No. UCD/CGM-14/01, Center for Geotechnical Modeling, Department of Civil and Environmental Engineering, University of California, Davis, CA, 134 pp. [3] Huang Q. 2014 Effect of nonplastic fines on cone resistance in silty sand, PhD Dissertation, University at Buffalo, Buffalo, NY. [4] Idriss, I. M. and Boulanger, R. W., 2008. "Soil liquefaction during earthquakes", Monograph MNO-12, Earthquake Engineering Research Institute, Oakland, CA, 261 pp. [5] Ishihara, K. (1993) “Liquefaction and flowfailureduring earthquakes” Geotechnique, Vol. 43(3), 351-441 [6] Kramer, S. L. and Seed, H. B. (1988) “Initiation of soil liquefaction under static loading conditions” J. of Geotech. Eng., ASCE, Vol. 114(4), 412-430 [7] Kramer, S. L. (1996), Geotechnical Earthquake Engineering, Prentice-Hall, Englewood Cliffs, NJ, 653p. [9] Randolph, M. F. and Hope, S., 2004. "Effect of cone velocity on the cone resistance and excess pore pressures", IS Osaka - Engineering Practice and Performance of Soft Deposits, Osaka, Japan, 147-152. [10] Robertson, P. K. and Campanella, R. G. (1985) “Liquefaction potential of sands using the CPT” Journal of Geotechnical Eng., Vol. 111(3), 384-403 [11] Robertson, P. K., and Wride (Fear), C. E.,1998. "Evaluating cyclic liquefaction potential using the cone penetration test", Canadian Geotechnical Journal, 35, 442–459. [12] Sivaratnarajah, U. 2016, Effect of non-plastic silt on cone resistance, MS Dissertation, University at Buffalo, Buffalo, NY,. [13] Seed H. B., Idriss, I. M., and Arango I.(1983).“Evaluation of liquefaction potential using fieldperformancedata.”J. Geotech. Eng., ASCE, 109(3): 458-482. [14] Seed, H. B., and De Alba, P. ,1986. "Use of SPT and CPT tests for evaluating the liquefactionresistanceofsands.’’ Proceeding, Speciality Conference on Use of In-Situ Testing in 88 [15] Shenthan, T. ,2001. "Factors affecting liquefaction mitigation in silty soils using stone columns", M.S. Thesis, State University of New York at Buffalo, NY. [16] Stark, T. D., and Olson, S. M., 1995. "Liquefaction resistance using CPT and field case histories.’’ Journal of Geotechnical Engineering, 121(12), 856–869. [17] Thevanayagam, S. (2000a) “Liquefaction potential and undrained fragility of silty soils” Proc. of the 12th Int. World Conf. on Earthquake Engineering, Auckland,New Zealand, 124-131 [18] Thevanayagam, S. (2000b) “Liquefaction in silty soils - Considerations forscreening andretrofitstrategies”2nd Workshop on Mitigation of Seismic Effects on Transportation Structures, Taipei, Taiwan [19] Thevanayagam, S. and Mohan,S.(2000a)“Intergranular state variables and stress-strain behavior of silty soils” Geotechnique, Vol. 50(1), 1-23 [20] Thevanayagam, S., Liang, J. and Shenthan, T. (2000b) “Contact index andliquefactionpotential analysisofsilty and gravely soils” Proc. 14th ASCE Engineering Mechanics Conference, Austin, TX. [21] Thevanayagam, S. and Martin, G. R. 2002. "Liquefaction in silty soils – screening and remediation issues ", Soil Dynamics and Earthquake Engineering, Vol. 22, 1035- 1042. [22] Thevanayagam, S., Shenthan, T., and Kanagalingam, T., (2003). Role of intergranular contacts on mechanisms causing liquefaction and slope failures in silty sands. Final Report, USGS Award No. 01HQGR0032 and 99HQGR0021; US Geological Survey, Department of Interior, USA, 396p. [23] Thevanayagam, S., Shenthan, T., Mohan, S., and Liang, J., 2002. "Undrained fragilityof cleansands,siltysandsand
  • 6. International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 06 Issue: 05 | May 2019 www.irjet.net p-ISSN: 2395-0072 © 2019, IRJET | Impact Factor value: 7.211 | ISO 9001:2008 Certified Journal | Page 5353 sandy silts", Journal of Geotechnical and Geoenvironmental Engineering, 128(10),849-859. [24]Youd, T.L., and Idriss, I.,M., 2001. "Liquefaction resistance of soils: summary report from 1996 NCEER and 1998 NCEER/NSF workshops on evaluation of liquefaction resistance of soils", Journal of Geotechnical and Geoenvironmental Engineering, 127(4), 297-31. BIOGRAPHIES Md. Selim Reza M.Sc. (University at Buffalo) Senior Lecturer, Uttara University Dhaka, Bangladesh Md. Sohel Rana B.Sc. (DUET, Bangladesh) Assistant Engineer, LGED, Bangladesh