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Present-Day Salt Regime in Reservoirs of the Manych River Basin

机译:曼彻奇河流域水库中的当今盐政权

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摘要

The reservoir system of the Manych River basin is located in the Kuma-Manych Depression of the southern Russian region, which is characterized by an arid climate, a shortage of water resources, and the development of salt marches and saline soils. The system extends in an almost latitudinal direction for a distance of over 300 km and includes the Proletarskoe (length 180 km, area 800 km~2, volume 2 km~3), Veselovskoe (length 90 km, area 250 km~2, volume 0.8 km~3), and Ust'-Manych (length 60 km, area 70 km~2, volume 0.1 km~3) reservoirs. Their average depth ranges from 2.5 to 3.0 m. The system gives rise to natural-economic and social problems. Most important among these basins is Lake Manych-Gudilo, which represents a shallow relict marine basin in the Proletarskoe Reservoir.
机译:曼彻奇河流域的水库系统位于俄罗斯南部地区的库玛-马尼奇De陷,其特征是干旱的气候,水资源短缺以及盐分行军和盐碱土壤的发展。该系统几乎沿纬度方向延伸超过300 km,包括Proletarskoe(长度180 km,面积800 km〜2,体积2 km〜3),Veselovskoe(长度90 km,面积250 km〜2,体积) 0.8 km〜3)和Ust'-Manych(长度60 km,面积70 km〜2,体积0.1 km〜3)水库。它们的平均深度为2.5至3.0 m。该系统引起自然经济和社会问题。在这些盆地中,最重要的是曼奇-古迪洛湖,它代表Proletarskoe水库中的浅水遗迹海洋盆地。

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