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Sediment is not a problem.
M. Detering and D. Bartelt
Abstract:
In many reservoirs and hydropower installations sediment is
seen as a problem which should be avoided, because a high
load of sediment in the outflow is causing wear on machinery.
Furthermore some ecologists fear clogging of interstitials when
passing on sediment. By seeing sediment as a problem in such
a way and blocking sediment transport, sediment accumulation
in reservoirs in the long run leads to even larger problems in
both cost and ecology. The only sustainable and
environmentally solution in the end is not to see sediment as a
problem, but to enable a cost efficient near-nature sediment
transport.
1 Introduction
In nature like rivers, passage of water, species and sediment was granted for millions
of years. Upon the construction of dams, this situation changed profoundly. Every
dam and reservoir - built for a reasonable and well considered technical use – also
implies an interruption for water flow, fish passage and foremost of sediment transfer.
Hydrology is well considered in reservoir planning. For low level dams fish passage
techniques are well established, for high dams in most cases it is no issue. But
sediment transfer in many cases is still neglected, despite the large problems
evolving from this.
2 The two sides of sediment
2.1 Sedimentation of reservoirs
By this, sooner or later every reservoir operator is faced with siltation in the reservoir.
As long as this sedimentation takes place within the dead storage, the operator might
not feel the need for action. But even then, the downstream river stretch is affected
as described in 2.2.
As soon as the sedimentation is reducing the active storage, also the reservoirs use
and thus the economics are affected. Because sedimentation is a sneaking process,
the problem of reduced storage is often transferred from generation to generation of
responsible staff, always considered ‘normal’. Psychologists refer to this development
as ‘shifting baseline’.
However, even under these circumstances operational and contractual obligations
have to be met, e.g. sufficient storage to ensure reserves, black start capability etc.
As conventional dredging is extremely costly and landfill is – if at any possible – a
further consumption of space, operators often accept sedimentation as long as
possible. The consequence of this development is shown in Figure 1.
Fig 1: Worldwide development of reservoirs and siltation (Source: DB Sediments)
Worldwide hydro storage volume is increases around 1 % per year by new build of
dams. At the same time 2 % of reservoir volume is lost due to sedimentation. As Fig.
1 clearly shows, this development is progressing. Without further action one quarter
of all dams in the next 25 to 50 years will lose their storage function by sedimentation
(WCD 2000). Sedimentation is probably the most serious technical problem faced by
the hydropower business.
As an assumed solution or compensation, many silted reservoirs are replaced by
new build of neighboring reservoirs. But this is clearly not sustainable as the
replacements will suffer the same problems only few decades later. Then at the
latest, room for even more reservoirs will not be available one day.
So far, operators tend to flush out sediment. For some installations, this might be
adequate if the downstream river does not bear any significant aquatic life. For the
most rivers, reservoir flushing causes the temporary coating of downstream river
stretches with often sediment of anaerobic quality. During flushing, hydraulics usually
allow only sediment close to the outlet or in a narrow ditch to be mobilized. The
sediment volume being mobilized is thus only a small fraction of the overall siltation.
The focus on flushing therefore is not on re-gaining storage volume, but to keep the
outlets operational before blocking becomes an irreversible problem.
As the flushing is being conducted during just a short time period of usually several
hours and the sediment transfer during this period is massive, the sediment transport
capacity of the downstream river as well as the rivers ability to handle a massive load
of anaerobic sediment is overstrained. Flushing therefore in many cases is to be
avoided from an ecological standpoint and unlawful in most European Countries.
2.2 Downstream river erosion
Sedimentation in reservoirs does not lead only to problems within the reservoir. Due
to the retention of sediment the important equilibrium within the river system is
disturbed. The lack of sediment in the downstream river causes a change of the bed
structure and massive erosion of the riverbed. This erosion can lead to immense
scale. The River Rhine e.g. faces a sediment deficit of 2.5 Million tons per year due
to sediment retention in its tributaries. One consequence is an annual erosion of 3 to
30 mm. Within only a few decades this will lead to required measures on harbors
along the Rhine and major construction works to ensure structural safety of hydro
and waterway installations.
To compensate for the most urgent damages on the riverbed the authorities actually
dump several hundred thousand tons of substitute material which is excavated on
land and which leads to further consume of space.
For these reasons the European Water Framework Directive (WFD) has identified not
only fish passage and hydrology, but also sediment transfer as a major aim, being
emphasized within the second WFD planning period. Unlike other elements of the
WFD, operators should understand that sediment transfer does bear long term cost
benefits, if applied in the right way.
3 Solutions
It could all be so easy. And in fact, it is. It begins with changing the view from
considering sediment a problem towards simply dealing with sediment as a standard
issue for reservoir operators. If reservoirs cause an imbalance in the sediment
transport, combined with problems upstream and/or downstream, why not set this
balance back where it belongs, especially if this can be done in a very cost efficient
way?
3.1 Analysis
As the hydrological and sediment situation varies from reservoir to reservoir, the first
step to develop a cost efficient sediment transfer should be to conduct a study. If
required, an actual bathymetry is performed. Most important part of the analysis is to
identify technical and environmental constraints with the core element being to
assess the transport capability of the downstream river stretch. The analysis also
gives information about the kind of applicable equipment and dimensioning.
3.2 Implementation
Given this information, the practical implementation can be prepared and installed. A
main difference to formerly dredging and landfill is that not disposal cost occur,
transportation is limited and the overall installation and application usually can be
performed without lowering the reservoir or even interrupting power generation.
Mechanical dewatering of the sediment is of course unnecessary, too (sample see
Fig. 2).
Fig. 2: Continuous Sediment Transfer at HPP Rodund/Austria (image source: DB Sediments)
In difference to dredging campaigns or flushing, the sediment outflow is not massive
during a short time, but smaller over a longer time period. This allows for smaller
equipment compared to conventional approaches (sample see Fig. 3).
Fig. 3: Sample for Sediment Transfer Equipment
The sediment transfer is performed according to the actual transport capability of the
downstream river. Thus, blocking of the riverbed system is prevented. If required, the
transferred sediment can also be vented to prevent a lack of oxygen in case of
massively anaerobe sediments. The sediment is given back to the river system in a
near-nature-way, allowing for erosion compensation.
4 Technical issues
Sediment transfer to the downstream river section can take place in different ways:
 through the turbines/power station
 through the base outlet or similar outlets
 over the dam
One of the first glance, many mechanical engineers fear the effects on sediment on
turbine abrasion if sediment is transferred across the power station. Damage on
turbine equipment can amount to a hundred thousand Euros and more. On the
second glance a transfer across the turbine for many applications still is the favorable
one for several reasons:
 additional abrasion usually is no or limited concern for heads below 200 m
 expenditures for turbine rehabs or even runner replacements sum up to just a
fraction of the cost saved in difference to conventional dredging, so in the end
this method still is very cost effective
 modern coating gives protection to runner surfaces (see Fig. 4)
 no water is wasted for sediment transfer
 not additional infrastructure is required
Fig. 4: WC-coated Francis Runner (left) and its labyrinth seal (right) after passage of 159,000 t of
abrasive sediment without significant abrasion effects (image source: University of Katmandu)
A recent development for pressure pipe desilting [4] could potentially accompany this
approach and make it applicable even for high head Pelton systems. By this, the
penstock would be used for sediment transfer and the majority of the sediment
removed before the turbine.
In case there are still concerns on a turbine passage, the sediment flow can also be
performed via other reservoir outlets or over the dam. However, in these cases often
additional equipment will be required which in the end still gives economic benefit.
5 Recommendations
With a different view on sedimentation issues, hydropower operators on the one hand
will find more economic solutions on reservoir maintenance and provide real
sustainability for their installations. By this, sediment transfer might be the only part of
the European Water Framework directive, granting operators a direct economic
benefit. On the other hand sediment transfer re-establishes an urgently needed
compensation for ongoing erosion for downstream river stretches, caused by a lack
of sediment in theses river sections.
Ongoing projects will ease the way to establish this ecological benefit as a standard
solution, also due to the lack of alternatives on many sites, according to: “If you think
sediment transfer is costly - try siltation.”
References
[1] Hr. Schüttrumpf and M. Detering: Innovative sediment handling to restore
reservoir capacity, Dams and reservoirs under changing challenges / Ed. by
Anton J. Schleiss, ISBN: 978-0-415-68267-1, pp 345- 352, 2011, CRC Press
[2] WCD: The Report of the World Commission on Dams, London/Sterling,
Earthscan Publications (2000)
[3] E. Doujak: Development of an Axial Hydro Cyclone for Pressure Pipe Desilting;
HydroVision 2011, 6 S.
Authors
Dr. Michael Detering
DB Sediments GmbH
Bismarckstr. 142, 47057 Duisburg, Germany
Phone +49 203 306-3625, Fax +49 203 306-3629, Mobile +49 177 8531100
E-mail: m.detering@db-sediments.com
Dr. Dietrich Bartelt
DB Sediments GmbH
Bismarckstr. 142, 47057 Duisburg, Germany
Phone +49 203 306-3626, Fax +49 203 306-3629, Mobile +49 152 29888321
E-mail: d.bartelt@db-sediments.com
ABOUT THE AUTHORS
Michael Detering graduated from German RWTH Aachen University of Technology
in 1995 with a master in mechanical engineering and also a commercial background.
Later he added a Doctors degree in civil & hydraulic engineering. Since then he has
been involved in almost any type of renewable generation but always with a strong
focus on hydropower. With on-site experience he conducted a number of projects,
rehabs and assessments. Being responsible for a major European Power Producer in
Hydro Asset Management for 82 plants in six European countries he took the entire
plant fleet back on a sustainably operated course whilst significantly increasing
profits. Michael Detering is co-founder and associate of DB Sediments. Besides his
business function he teaches at Aachen University of Technology and contributes to
several technical associations, including ICOLD and its TC Environment.
Dietrich Bartelt studied civil engineering and business administration at Aachen
University of Technology (RWTH Aachen), Germany. He specialized in hydraulic
engineering, water resources management, soil mechanics and environmental
management. Since 1992 he has been working for a major European Utility and held
various technical and management positions. As Senior Manager he was responsible
for the coordination of environmental issues for several hundred companies of the
Group. In 2012 he published his doctor thesis on “trust of employees’ in their
management”. In the fields of renewable power generation, he has been active in
setting up multi-national projects, project management structures, site development,
authorization procedures, plant operations, and joint implementation projects with a
focus on hydropower. He is associate of DB Sediments.

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141209 2014 ViennaHydro Paper Detering Bartelt Sediment

  • 1. Sediment is not a problem. M. Detering and D. Bartelt Abstract: In many reservoirs and hydropower installations sediment is seen as a problem which should be avoided, because a high load of sediment in the outflow is causing wear on machinery. Furthermore some ecologists fear clogging of interstitials when passing on sediment. By seeing sediment as a problem in such a way and blocking sediment transport, sediment accumulation in reservoirs in the long run leads to even larger problems in both cost and ecology. The only sustainable and environmentally solution in the end is not to see sediment as a problem, but to enable a cost efficient near-nature sediment transport. 1 Introduction In nature like rivers, passage of water, species and sediment was granted for millions of years. Upon the construction of dams, this situation changed profoundly. Every dam and reservoir - built for a reasonable and well considered technical use – also implies an interruption for water flow, fish passage and foremost of sediment transfer. Hydrology is well considered in reservoir planning. For low level dams fish passage techniques are well established, for high dams in most cases it is no issue. But sediment transfer in many cases is still neglected, despite the large problems evolving from this. 2 The two sides of sediment 2.1 Sedimentation of reservoirs By this, sooner or later every reservoir operator is faced with siltation in the reservoir. As long as this sedimentation takes place within the dead storage, the operator might not feel the need for action. But even then, the downstream river stretch is affected as described in 2.2. As soon as the sedimentation is reducing the active storage, also the reservoirs use and thus the economics are affected. Because sedimentation is a sneaking process, the problem of reduced storage is often transferred from generation to generation of responsible staff, always considered ‘normal’. Psychologists refer to this development as ‘shifting baseline’.
  • 2. However, even under these circumstances operational and contractual obligations have to be met, e.g. sufficient storage to ensure reserves, black start capability etc. As conventional dredging is extremely costly and landfill is – if at any possible – a further consumption of space, operators often accept sedimentation as long as possible. The consequence of this development is shown in Figure 1. Fig 1: Worldwide development of reservoirs and siltation (Source: DB Sediments) Worldwide hydro storage volume is increases around 1 % per year by new build of dams. At the same time 2 % of reservoir volume is lost due to sedimentation. As Fig. 1 clearly shows, this development is progressing. Without further action one quarter of all dams in the next 25 to 50 years will lose their storage function by sedimentation (WCD 2000). Sedimentation is probably the most serious technical problem faced by the hydropower business. As an assumed solution or compensation, many silted reservoirs are replaced by new build of neighboring reservoirs. But this is clearly not sustainable as the replacements will suffer the same problems only few decades later. Then at the latest, room for even more reservoirs will not be available one day. So far, operators tend to flush out sediment. For some installations, this might be adequate if the downstream river does not bear any significant aquatic life. For the most rivers, reservoir flushing causes the temporary coating of downstream river stretches with often sediment of anaerobic quality. During flushing, hydraulics usually
  • 3. allow only sediment close to the outlet or in a narrow ditch to be mobilized. The sediment volume being mobilized is thus only a small fraction of the overall siltation. The focus on flushing therefore is not on re-gaining storage volume, but to keep the outlets operational before blocking becomes an irreversible problem. As the flushing is being conducted during just a short time period of usually several hours and the sediment transfer during this period is massive, the sediment transport capacity of the downstream river as well as the rivers ability to handle a massive load of anaerobic sediment is overstrained. Flushing therefore in many cases is to be avoided from an ecological standpoint and unlawful in most European Countries. 2.2 Downstream river erosion Sedimentation in reservoirs does not lead only to problems within the reservoir. Due to the retention of sediment the important equilibrium within the river system is disturbed. The lack of sediment in the downstream river causes a change of the bed structure and massive erosion of the riverbed. This erosion can lead to immense scale. The River Rhine e.g. faces a sediment deficit of 2.5 Million tons per year due to sediment retention in its tributaries. One consequence is an annual erosion of 3 to 30 mm. Within only a few decades this will lead to required measures on harbors along the Rhine and major construction works to ensure structural safety of hydro and waterway installations. To compensate for the most urgent damages on the riverbed the authorities actually dump several hundred thousand tons of substitute material which is excavated on land and which leads to further consume of space. For these reasons the European Water Framework Directive (WFD) has identified not only fish passage and hydrology, but also sediment transfer as a major aim, being emphasized within the second WFD planning period. Unlike other elements of the WFD, operators should understand that sediment transfer does bear long term cost benefits, if applied in the right way. 3 Solutions It could all be so easy. And in fact, it is. It begins with changing the view from considering sediment a problem towards simply dealing with sediment as a standard issue for reservoir operators. If reservoirs cause an imbalance in the sediment transport, combined with problems upstream and/or downstream, why not set this balance back where it belongs, especially if this can be done in a very cost efficient way? 3.1 Analysis As the hydrological and sediment situation varies from reservoir to reservoir, the first step to develop a cost efficient sediment transfer should be to conduct a study. If
  • 4. required, an actual bathymetry is performed. Most important part of the analysis is to identify technical and environmental constraints with the core element being to assess the transport capability of the downstream river stretch. The analysis also gives information about the kind of applicable equipment and dimensioning. 3.2 Implementation Given this information, the practical implementation can be prepared and installed. A main difference to formerly dredging and landfill is that not disposal cost occur, transportation is limited and the overall installation and application usually can be performed without lowering the reservoir or even interrupting power generation. Mechanical dewatering of the sediment is of course unnecessary, too (sample see Fig. 2). Fig. 2: Continuous Sediment Transfer at HPP Rodund/Austria (image source: DB Sediments) In difference to dredging campaigns or flushing, the sediment outflow is not massive during a short time, but smaller over a longer time period. This allows for smaller equipment compared to conventional approaches (sample see Fig. 3).
  • 5. Fig. 3: Sample for Sediment Transfer Equipment The sediment transfer is performed according to the actual transport capability of the downstream river. Thus, blocking of the riverbed system is prevented. If required, the transferred sediment can also be vented to prevent a lack of oxygen in case of massively anaerobe sediments. The sediment is given back to the river system in a near-nature-way, allowing for erosion compensation. 4 Technical issues Sediment transfer to the downstream river section can take place in different ways:  through the turbines/power station  through the base outlet or similar outlets  over the dam One of the first glance, many mechanical engineers fear the effects on sediment on turbine abrasion if sediment is transferred across the power station. Damage on turbine equipment can amount to a hundred thousand Euros and more. On the second glance a transfer across the turbine for many applications still is the favorable one for several reasons:  additional abrasion usually is no or limited concern for heads below 200 m  expenditures for turbine rehabs or even runner replacements sum up to just a fraction of the cost saved in difference to conventional dredging, so in the end this method still is very cost effective  modern coating gives protection to runner surfaces (see Fig. 4)  no water is wasted for sediment transfer  not additional infrastructure is required
  • 6. Fig. 4: WC-coated Francis Runner (left) and its labyrinth seal (right) after passage of 159,000 t of abrasive sediment without significant abrasion effects (image source: University of Katmandu) A recent development for pressure pipe desilting [4] could potentially accompany this approach and make it applicable even for high head Pelton systems. By this, the penstock would be used for sediment transfer and the majority of the sediment removed before the turbine. In case there are still concerns on a turbine passage, the sediment flow can also be performed via other reservoir outlets or over the dam. However, in these cases often additional equipment will be required which in the end still gives economic benefit. 5 Recommendations With a different view on sedimentation issues, hydropower operators on the one hand will find more economic solutions on reservoir maintenance and provide real sustainability for their installations. By this, sediment transfer might be the only part of the European Water Framework directive, granting operators a direct economic benefit. On the other hand sediment transfer re-establishes an urgently needed compensation for ongoing erosion for downstream river stretches, caused by a lack of sediment in theses river sections. Ongoing projects will ease the way to establish this ecological benefit as a standard solution, also due to the lack of alternatives on many sites, according to: “If you think sediment transfer is costly - try siltation.” References [1] Hr. Schüttrumpf and M. Detering: Innovative sediment handling to restore reservoir capacity, Dams and reservoirs under changing challenges / Ed. by Anton J. Schleiss, ISBN: 978-0-415-68267-1, pp 345- 352, 2011, CRC Press [2] WCD: The Report of the World Commission on Dams, London/Sterling, Earthscan Publications (2000) [3] E. Doujak: Development of an Axial Hydro Cyclone for Pressure Pipe Desilting; HydroVision 2011, 6 S.
  • 7. Authors Dr. Michael Detering DB Sediments GmbH Bismarckstr. 142, 47057 Duisburg, Germany Phone +49 203 306-3625, Fax +49 203 306-3629, Mobile +49 177 8531100 E-mail: m.detering@db-sediments.com Dr. Dietrich Bartelt DB Sediments GmbH Bismarckstr. 142, 47057 Duisburg, Germany Phone +49 203 306-3626, Fax +49 203 306-3629, Mobile +49 152 29888321 E-mail: d.bartelt@db-sediments.com ABOUT THE AUTHORS Michael Detering graduated from German RWTH Aachen University of Technology in 1995 with a master in mechanical engineering and also a commercial background. Later he added a Doctors degree in civil & hydraulic engineering. Since then he has been involved in almost any type of renewable generation but always with a strong focus on hydropower. With on-site experience he conducted a number of projects, rehabs and assessments. Being responsible for a major European Power Producer in Hydro Asset Management for 82 plants in six European countries he took the entire plant fleet back on a sustainably operated course whilst significantly increasing profits. Michael Detering is co-founder and associate of DB Sediments. Besides his business function he teaches at Aachen University of Technology and contributes to several technical associations, including ICOLD and its TC Environment. Dietrich Bartelt studied civil engineering and business administration at Aachen University of Technology (RWTH Aachen), Germany. He specialized in hydraulic engineering, water resources management, soil mechanics and environmental management. Since 1992 he has been working for a major European Utility and held various technical and management positions. As Senior Manager he was responsible for the coordination of environmental issues for several hundred companies of the Group. In 2012 he published his doctor thesis on “trust of employees’ in their management”. In the fields of renewable power generation, he has been active in setting up multi-national projects, project management structures, site development, authorization procedures, plant operations, and joint implementation projects with a focus on hydropower. He is associate of DB Sediments.