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Chapter 29 On Some Issues of the Anthropogenic Transformation of Water Ecosystems (Case Study of Lake Sevan)

机译:第29章关于水生态系统人为转变的若干问题(塞凡湖案例研究)

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This paper discusses the influence of economic development in the basin of Lake Sevan. It shows that the decrease of lake's water level has led to changes in the hydrological regime. The development in the basin has caused disruption of thermal and hydro-chemical regimes of the lake, deteriorating the water quality and increasing the water turbidity. The circulation of biological and chemical species has changed as well. Studies of the chemical composition of the water were launched at the end of the nineteenth century, and the first salt balance was determined in the 1930s. According to routine observations, 1 1 of the lake's water contains about 0.7 g salt in ionic form, which has changed by about 5-10% as a result of the decrease of water level. There have been changes in the general mineralization that are related to the decrease of the water level and the magnitude of its flow. In 1928-1930, well before artificial changes to the lake's water level were realized, the total mineralization was 718.4 mg/1, while today it is 673 mg/1 (1999-2002). The decrease of total general mineralization of lake water is strongly related to the massive outflow of salty water, which removed salts that have been accumulating in the lake for centuries. The studies of separate components of Lake Sevan balance show that under conditions of the global climate warming, evaporation from the lake's surface may reach up to 145 × 10~6 m~3/annum. Averaging of the consequences of possible climate change on river runoff points at the possible decrease of water resources of the lake's basin by -2.51 % by the end of the first half of the twenty-first century. It is hard to predict the future developments of these processes. However, the issue of Lake Sevan is not entirely settled as the ecosystem of the lake is damaged and is undergoing the process of eutrophication. The flora and fauna of the water and coast have undergone serious and irreversible changes.
机译:本文讨论了塞凡湖流域经济发展的影响。这表明湖泊水位的下降导致水文状况的变化。流域的发展已导致湖泊的热化学和水化学状态中断,水质恶化,水浊度增加。生化物种的流通也发生了变化。在19世纪末开始研究水的化学成分,并在1930年代确定了第一个盐平衡。根据常规观察,湖水中的1 1含有约0.7 g离子形式的盐,由于水位降低,盐的含量已改变约5-10%。总体矿化发生了变化,这与水位的下降及其流量的大小有关。在1928年至1930年,在未实现对湖水位进行人工更改之前,总矿化度为718.4 mg / 1,而今天为673 mg / 1(1999-2002年)。湖泊水总矿化总量的减少与咸水的大量流出密切相关,咸水大量流失了盐湖中已有数百年的盐分。对塞凡湖天平的各个组成部分的研究表明,在全球气候变暖的条件下,湖面的蒸发量可能达到每年145×10〜6 m〜3 /年。平均气候变化对河流径流点的影响,到二十世纪上半叶末,湖盆的水资源可能减少-2.51%。很难预测这些过程的未来发展。但是,塞凡湖的问题尚未完全解决,因为该湖的生态系统受到了破坏,正在经历富营养化的过程。水和海岸的动植物发生了严重且不可逆转的变化。

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