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Simulating dam removal with a ID hydraulic model: Accuracy and techniques for reservoir erosion and downstream deposition at the Chiloquin Dam removal

机译:使用ID水力模型模拟大坝拆除:Chiloquin大坝拆除时储层侵蚀和下游沉积的精度和技术

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Hydrodynamic models are often used to reduce uncertainty regarding the outcomes of dam removal, though the accuracy of these models is not regularly evaluated post-removal. With the goal of improving understanding on the accuracy and limitations of making predictions of sediment dynamics following dam removal, we compare predicted and observed sediment erosion and deposition in the reservoir and downstream for the Chiloquin Dam removal. Results from a ID (HEC-RAS) hydraulic and sediment transport analysis (Yang equation) are compared to pre- and post-removal bathymetric and sediment surveys. Observed bathymetric changes indicate minimal response in both the reservoir and the downstream reaches to the removal, due in part to the low water year and the low volume of sediment stored in the reservoir following drawdown. Model simulations overpredicted erosion in the reservoir and downstream relative to what was observed, likely due to a combination of limited field documentation of resistant hardpan and to issues in model stability. Magnitude and potential sources of error are presented and suggestions are made regarding data needs and potential modeling approaches in future dam removal studies.
机译:水动力模型通常用于减少有关大坝拆除结果的不确定性,尽管这些模型的准确性并未在拆除后定期评估。为了增进对拆除大坝后泥沙动力学预测的准确性和局限性的理解,我们比较了Chiloquin大坝拆除后在储层和下游的预测和观察到的泥沙侵蚀和沉积。将ID(HEC-RAS)水力和泥沙输送分析(Yang方程)的结果与拆卸前后的测深和泥沙调查进行比较。测得的测深变化表明,在水库和下游对清除的响应最小,部分原因是水位低和水位下降后水库中存储的沉积物量少。相对于所观察到的结果,模型模拟高估了储层和下游的侵蚀,这可能是由于有限的抗硬壳实地记录和模型稳定性问题的综合作用所致。介绍了误差的大小和潜在来源,并就未来大坝拆除研究中的数据需求和潜在的建模方法提出了建议。

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