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Jezioro Aralskie – największa katastrofa ekologiczna minionego stulecia

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Jezioro Aralskie... (313.4Kb)
Author:
Bielecki, Rafał
xmlui.dri2xhtml.METS-1.0.item-citation: Annales Universitatis Paedagogicae Cracoviensis. 93, Studia Geographica 1 (2010), s. [6]-13
xmlui.dri2xhtml.METS-1.0.item-iso: pl
Subject:
relict lake
Amu-Darya delta
Syr-Darya delta
irrigation channels
deserfitication
Date: 2010
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Abstract
One of the best examples of environmental risk arising as a result of inefficient management of environmental resources is the disappearance of the Aral Sea. Aral Sea extends into the territories of Kazakhstan and Uzbekistan. About 10 thousand years ago, this vast body of water was under the influence of water from melting mountain glaciers, flowing directly into the Aral Basin. However, the climate change which started about 3500 years ago contributed to the drying process of the tank. This process became stronger in character at the beginning of the 1960s, when due to the planned economy of the USSR, it was decided to develop large-scale cultivation of cotton in areas too dry to be suitable for such crops. Therefore, the water from the rivers Syr-Darya and Amu-Darya, flowing into the Aral Sea, was directed to irrigation, without worrying about the ecological balance. Consequently, this led to irreversible environmental changes. The Aral Sea Area decreased by 40% and its volume decreased by two-thirds. Water level dropped about 13 feet and is still falling. Historically, the reservoir was fed by more than 60 km3 of water per year; currently it is only about 5 km3. There were years when the lake received virtually no water as a result of these processes. In 1988 a division of the lake into two parts was carried out: the Big Aral Sea in the south and the Small Aral Sea in the north. The salinity of water remaining in the basin has increased roughly threefold, which has disastrous consequences for the world’s flora and fauna. The Aral Sea region’s economy disappeared completely, e.g. the fisheries and associated processing industries, as in water with such high salt content no organisms are able to survive. As the lake shrank and large parts of it are now dry, when strong winds blow across the land, they carry huge amounts of tiny particles of salt remaining after the water has evaporated. It has been calculated that in the year after such a dust storm around 75 million tonnes of sand mixed with salt was spread. The toxic dust destroys settlings, fields, and plants, and it is difficult to find a way to counteract this process.
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http://hdl.handle.net/11716/11700
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Budowa Repozytorium Uniwersytetu Komisji Edukacji Narodowej w Krakowie została sfinansowana ze środków Ministerstwa Nauki i Szkolnictwa Wyższego na działalność upowszechniającą naukę.

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