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The influence of water level fluctuations in the Ust-Ilimsk water reservoir in Russia on the action of some geological processes

机译:俄罗斯乌斯季-伊利姆斯克水库水位波动对某些地质过程作用的影响

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The Ust-Ilimsk water reservoir is located in the taiga zone in the Central-Siberian Upland. It was created between 1975-1977 as a result of storage of flood waters and water from the higher located Bratsk Reservoir. With an area of 1873 km2 and a water capacity amounting to 59.4 km3 it belongs to the group of largest water reservoirs in the world. It is the third level of the Angara cascade, projected as a multifunctional object - for the efficient functioning of the Ust-Ilimsk Hydroelectric Power Station, to streamline navigation on the lower Angara, to fulfil municipal and industrial water needs and also for floating timber. On the basis of the author’s own investigations and source materials obtained from the Irkutskgidromet and the Institute of the Earth’s Crust in Irkutsk, the fluctuations of the water level and the volumes of water outflow in the period 1975-2007 and the volume of processed material at the selected water shores in the period 1977-1990 were analysed. In addition, the data of seismic events in the region of the Ust-Ilimsk water reservoir were compiled. During this period the functioning changes of the reservoir in terms of the capacity of the water mass occurred under the influence of both natural and anthropogenic factors. It was determined that the creation of this natural-technical water object activated two geological processes in its shore zone - abrasion and induced seismicity. It was stated that the especially large transformations of the reservoir shore zone by these dangerous processes occurred in the first years of its intensive exploitation, in the period of small water resources in the drainage basin of Yenisei - Angara, which forced specific conditions of reservoir functioning. At rocky shores the predominating process is abrasion of their waterside parts, whereas at shores built of loose deposits the complete transformation of underwater parts of shallows takes place.
机译:Ust-Ilimsk水库位于中西伯利亚山地的taiga地区。它是在1975年至1977年之间储存洪水和来自较高位置的布拉茨克水库的水而创建的。它是世界上最大的水库群,总面积为1873平方公里,水容量为59.4平方千米。它是安加拉小瀑布的第三层,预计将作为一个多功能对象-用于乌斯特-伊利姆斯克水电站的有效运行,精简安加拉河下游的航行,以满足市政和工业用水的需求,还用于浮木。根据作者自己的调查和从伊尔库茨克研究中心和伊尔库茨克地壳研究所获得的原始资料,1975-2007年期间的水位和出水量的波动以及分析了1977-1990年期间选定的水岸。此外,还编辑了乌斯特-伊利姆斯克水库地区的地震事件数据。在此期间,在自然因素和人为因素的共同作用下,水库的功能发生了水量变化。可以确定的是,这种自然技术水物体的产生激活了其海岸带的两个地质过程-磨损和诱发地震。据指出,这些危险过程对水库岸域的特别大的变化发生在其集约开发的头几年,在叶尼塞—安加拉河流域的水资源较少的时期,这迫使水库发挥特定的作用条件。 。在多岩石的海岸上,主要的过程是对其水边部分的磨损,而在由松散的沉积物建造的海岸上,浅水区的水下部分发生了完全转变。

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