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首页> 外文期刊>International association of theoretical and applied limnoloy >Pioneer limnological observations on the developed ecosystem of a permanent lake in Abu-Dhabi Desert, U.A.E
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Pioneer limnological observations on the developed ecosystem of a permanent lake in Abu-Dhabi Desert, U.A.E

机译:阿联酋阿布扎比沙漠中一个永久性湖泊发达生态系统的先驱物学观测

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摘要

In arid regions, wetlands and salt lakes are the most productive environments, whether natural or man-made. In these environments, water is the primary factor influencing plant and animal life (WILLIAMS 1993, 1998, SADA 2001, ZHENG 2001). Despite its subtropical arid nature, the Gulf region hosts several wetlands represented by the mangrove environments of the coastal areas. These wetlands are in stark contrast to the remainder of the Arabian Peninsula, which is characterized by deserts with ephemeral salt lakes that form immediately after rainfalls on low-lying areas with hypersaline substrates. In these latter environments, there are no permanent all-season saline lakes. However, in 1982 a permanent lake formed within the desert of Abu-Dhabi (largest emirate of the United Arab Emirates), due to an unplanned discharge of secondary treated wastewater from Al-Marfaq sewage treatment plant into a neighbouring area of sabkha. Subsequent small discharges have maintained the lake as a permanent body of water. The lake is fed by the continuous supply of treated water and also by saline drainage and runoff from the nearby Al-Wathba Camel Race Track. Evaporation is the main factor responsible for the water level decrease of the lake. Daily evaporation varies between 8000 m~3 in winter and 22 000 m~3 in summer.
机译:在干旱地区,无论是自然的还是人为的,湿地和盐湖都是生产力最高的环境。在这些环境中,水是影响动植物生命的主要因素(WILLIAMS 1993,1998,SADA 2001,ZHENG 2001)。尽管它具有亚热带干旱的性质,但海湾地区还是拥有一些以沿海地区的红树林环境为代表的湿地。这些湿地与阿拉伯半岛的其余部分形成鲜明对比,阿拉伯半岛的其余部分的特点是沙漠中带有短暂盐湖,这些盐湖在高盐含量低洼地区降雨后立即形成。在后面这些环境中,没有永久性的全季节盐湖。但是,由于计划外的二次处理废水从Al-Marfaq污水处理厂向计划外的sabkha地区排放,1982年在阿布扎比沙漠(阿拉伯联合酋长国最大的酋长国)内形成了一个永久性湖泊。随后的少量排放使该湖成为永久的水体。不断供应处理过的水,以及附近的Al-Wathba骆驼赛道的盐水排泄和径流,为该湖提供了食物。蒸发是导致湖泊水位下降的主要因素。冬季每天的蒸发量在8000 m〜3之间,而夏季则为22000 m〜3。

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