基于水动力模型的大型水电设施下游大规模生产砂砾混合料可能后果分析(以Votkinsk水电站为例)

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引用次数: 0

摘要

作者在考虑已建立的水体水动力模型的基础上,通过多版本计算试验,对下卡玛水库(Votkinsk水库下游)上部大规模开采砂砾混合料可能产生的水力后果进行了估计。这种估计对于制定旨在尽量减少负面后果和在用水者之间提供利益平衡的措施是必要的。方法。这项工作是基于一组现场观测与基于一维和二维公式的水动力学模型的计算实验的结合,这使得对高压发电站的释放波进行水动力学计算成为可能。结果。研究了不同计算场景下的水位动态,并根据2019年自然条件下的一、二维形态测量模型计算结果,考虑砂砾石混合物沉积物的发育情况,绘制了水位对比图。实验表明,只有八个矿床(Volkovsk, Olkhovsk, Sivinsk, Golyanovo, Makarovsk,上杜莱索夫斯克,Simonikhinsk和Simonikhinsk-2)的开发将导致必须(为了保持3.3米的航行深度)将Votkinsk HPP下游的流量增加到1800立方米/秒或保持连续1500立方米/秒的流量至少24小时。在水位图对比分析过程中,在一维和二维建模中,可以区分出3个由于大规模开采砂/砾石混合物导致的高度沉降较大(15-41 cm)的位置。
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Analysis of the Possible Consequences of Large-Scale Production of Sand and Gravel Mixture in the Downstream of Large Hydroelectric Facilities Based on Hydrodynamic Modeling (the Votkinsk HPP as an Example)
The authors have presented estimation of possible hydraulic consequences of the large-scale mining of sand/gravel mixtures in the upper part of the Lower Kama Reservoir 9the Votkinsk Reservoir downstream) based on the multi-version computation experiments with the developed hydro/dynamic model of the water body under consideration. This estimation is necessary for development of measures aimed at minimization of negative aftermath and provision of the interest balance between water users. Methods. The work is based on the conjugation of a set of field observations with computational experiments based on hydrodynamic models in 1D and 2D formulations, which make it possible to carry out hydrodynamic calculations for the waves of releases from HPPs. Results. The dynamics of water levels was investigated for various calculation scenarios, graphs were drawn for comparing water levels based on the results of calculations in one- and two-dimensional models for morphometry in 2019 in natural conditions and taking into account the development of deposits of sand and gravel mixtures. The experiments have demonstrated that development of only eight deposits (Volkovsk, Olkhovsk, Sivinsk, Golyanovo, Makarovsk, Upper-Dulesovsk, Simonikhinsk, and Simonikhinsk-2) will cause the necessity (in order to maintain the 3.3 m navigation depth) to increase the discharge to the Votkinsk HPP downstream up to 1800 m3/s or maintaining of continuous 1500 m3/s discharge for at least 24 hours. In the process of the water level graphs comparative analysis, both in one-dimension and two-dimension modeling, one can distinguish three sites with great level subsidence (15-41 cm) due to the large-scale mining of sand/gravel mixture.
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