TY - JOUR
T1 - Dam Removal Express Assessment Models (DREAM). Part 2
T2 - Sample runs/sensitivity tests
AU - Cui, Yantao
AU - Braudrick, Christian
AU - Dietrich, William E.
AU - Cluer, Brian
AU - Parker, Gary
N1 - Funding Information:
Model development was partially supported by National Oceanic and Atmospheric Administration (NOAA). The following funding to Stillwater Sciences, the University of Minnesota, and University of California, Berkeley that directly or indirectly benefited the development of the current models are acknowledged: Portland General Electric (PGE), PacifiCorp, National Science Foundation (NSF), Environmental Protection Agency (EPA), National Aviation and Space Administration (NASA), Ok Tedi Mining Limited (OTML Papua New Guinea), St. Johns River Water Management District (Florida). We thank Drs. Marcelo Garcia (U Illinois), Thomas Lisle (USFS), James Pizzuto (U Delaware) and Stephen Wiele (USGS), whose reviews to the Marmot Dam removal modeling sparked many improvements in the development of the current models. Many Stillwater employees contributed to the development of the models, including Andrew Wilcox (now with Colorado State University), Frank Ligon, JenniferVick(nowwithMcBainandTrush), JohnO’Brien (now with US Forest Service), and Bruce Orr. Peter Downs reviewed an earlier draft and provided many useful suggestions. This paper is a contribution of the National Center for Earth-surface Dynamics (NCED) based at St. Anthony Falls Laboratory, University of Minnesota, in which the University of California, Berkeley participates, and of which Stillwater Sciences, Berkeley, California is a partner. The useful suggestions from two anonymous reviewers have been incorporated into the manuscript.
PY - 2006
Y1 - 2006
N2 - This paper presents sample runs of the Dam Removal Express Assessment Models (DREAM) presented in the companion paper, Cui et al. (2006): DREAM-1 for simulation of sediment transport following the removal of a dam behind which the reservoir deposit is composed primarily of non-cohesive sand and silt, and DREAM-2 for simulation of sediment transport following the removal of a dam behind which the upper layer of the reservoir deposit is composed primarily of gravel. The primary purposes of the sample runs presented here are to validate some of the assumptions used in the model and to provide guidance as how accurately the field data should be collected. Sample runs indicate that grain size distribution of the reservoir sediment deposit is the most important piece of information needed during the field campaign. Other than the grain size distribution of the reservoir sediment deposit, errors within a reasonable range in other parameters, do not result in significant variations in the predicted depositional patterns downstream of the dam, although different magnitudes of sediment deposition may result from such errors. Sample runs also indicate that when the reservoir deposit is composed primarily of gravel, sediment deposition downstream of the dam following dam removal may not propagate far downstream of the dam, and may be limited to isolated reaches where sediment transport capacity is low. Farther downstream sediment deposition becomes progressively smaller due to the attenuation of sediment transport and gravel abrasion. When the reservoir deposit is primarily fine sediment, however, there may be more extensive sediment deposition (both larger area and higher magnitude) downstream of the dam following dam removal. Dredging part of the sediment in advance reduces the downstream impact due to the reduced volume, and the extra distance provided by dredging allows for attenuation of sediment transport. Sample runs with staged dam removal indicate that it provides only limited benefit compared to a one-time removal in case the reservoir deposit is composed primarily of coarse sediment, but may provide significant benefits in case the reservoir deposit is composed primarily of fine sediment. The benefits of a staged removal for the latter case include reduced magnitude and area of deposition as well as reduced suspended sediment concentration downstream of the dam.
AB - This paper presents sample runs of the Dam Removal Express Assessment Models (DREAM) presented in the companion paper, Cui et al. (2006): DREAM-1 for simulation of sediment transport following the removal of a dam behind which the reservoir deposit is composed primarily of non-cohesive sand and silt, and DREAM-2 for simulation of sediment transport following the removal of a dam behind which the upper layer of the reservoir deposit is composed primarily of gravel. The primary purposes of the sample runs presented here are to validate some of the assumptions used in the model and to provide guidance as how accurately the field data should be collected. Sample runs indicate that grain size distribution of the reservoir sediment deposit is the most important piece of information needed during the field campaign. Other than the grain size distribution of the reservoir sediment deposit, errors within a reasonable range in other parameters, do not result in significant variations in the predicted depositional patterns downstream of the dam, although different magnitudes of sediment deposition may result from such errors. Sample runs also indicate that when the reservoir deposit is composed primarily of gravel, sediment deposition downstream of the dam following dam removal may not propagate far downstream of the dam, and may be limited to isolated reaches where sediment transport capacity is low. Farther downstream sediment deposition becomes progressively smaller due to the attenuation of sediment transport and gravel abrasion. When the reservoir deposit is primarily fine sediment, however, there may be more extensive sediment deposition (both larger area and higher magnitude) downstream of the dam following dam removal. Dredging part of the sediment in advance reduces the downstream impact due to the reduced volume, and the extra distance provided by dredging allows for attenuation of sediment transport. Sample runs with staged dam removal indicate that it provides only limited benefit compared to a one-time removal in case the reservoir deposit is composed primarily of coarse sediment, but may provide significant benefits in case the reservoir deposit is composed primarily of fine sediment. The benefits of a staged removal for the latter case include reduced magnitude and area of deposition as well as reduced suspended sediment concentration downstream of the dam.
KW - Dam decommissioning
KW - Dam removal
KW - Numerical model
KW - Sediment transport
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U2 - 10.1080/00221686.2006.9521684
DO - 10.1080/00221686.2006.9521684
M3 - Article
AN - SCOPUS:33746924553
SN - 0022-1686
VL - 44
SP - 308
EP - 323
JO - Journal of Hydraulic Research
JF - Journal of Hydraulic Research
IS - 3
ER -