克拉斯诺达尔水库淤积的新数据

A. Pogorelov, A. Laguta, E. Kiselev
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引用次数: 2

摘要

本文分析了克拉斯诺达尔水库淤积的空间特征和长期动态。克拉斯诺达尔水库是克拉斯诺达尔地区整个围垦系统的重点对象,年灌溉水量为33.5亿m3;分析是基于水深测量数据。必须对淤积量和水库水文特征的变化作出准确和最新的估计,以便为该区域的水资源消耗制订正确的长期战略。自1973年投入使用以来,水库发生了明显的变化:库班河和贝拉亚河的沉积物形成了一个广泛的屏障,水库分为两个独立的水库,而且变化还在继续。利用2005年、2016年和2021年的水深测量数据,计算了克拉斯诺达尔水库的淤积量和水文特征。我们已经确定,考虑到独立的Tshchikskoe水库和已经形成的桥梁,在2005年至2021年期间,镜面在正常保留水平的面积从382平方公里减少到224.2平方公里,而有用体积从1,606减少到12.704亿立方米。同期,死亡水量从1.92亿立方米减少到1.351亿立方米。在两次深海测量之间,淤积量达2466万立方米;2016-2021年的平均淤积率(493万m3)低于2005-2016年的平均值(686万m3)。在上一次调查期间,淤泥层的背景厚度约为0.1 m,其最大值(1-3 m以上)出现在突出的库班三角洲下方,长度超过2 km。
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NEW DATA ON SILTING OF THE KRASNODAR RESERVOIR
The paper analyzes spatial features and long-term dynamics of silting of the Krasnodar Reservoir, the key object of the entire reclamation system of the Krasnodar region with a 3.35 billion m3 annual limit of water intake for irrigation; the analysis is based on bathymetric survey data. Accurate and up-to-date estimates of siltation volumes and changes in the hydrometric characteristics of the reservoir are necessary to develop a correct long-term strategy for the consumption of water resources in the region. The reservoir has noticeably transformed since it was put into operation in 1973: it has divided into two independent reservoirs with the formation of an extensive barrier from sediments of the Kuban and Belaya rivers, and transformations are continuing. Bathymetric surveys of 2005, 2016, and 2021 were used to calculate the volumes of silting and hydrometric characteristics of the Krasnodar Reservoir. We have established that, taking into account the detached Tshchikskoe Reservoir and the bridge that has formed, over the period 2005–2021 the area of the mirror at a normal retaining level decreased from 382 to 224.2 km2, while the useful volume diminished from 1,606 to 1,270.4 million m3. Over the same period, the dead volume decreased from 192 to 135.1 million m3. During the period between the last bathymetric surveys, the volume of siltation amounted to 24.66 million m3; the average siltation rate for 2016–2021 (4.93 million m3) was found to be lower than the average value for 2005–2016 (6.86 million m3). With a background thickness of the silt layer of about 0.1 m for the period between the last surveys, its greatest values (1–3 m and more) were noted below the protruding Kuban delta at a section of more than 2 km long.
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