节点文献

艾比湖面积变化及对生态环境影响

Change in Ebinur Lake Area and Its Impact on Eco-environment

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 苏宏超巴音查汗庞春花吉锦环

【Author】 SU Hong-chao~1, BAYIN Cha-han~2, PANG Chun-hua~1, JI Jin-huan~3 (1.Xinjiang Hydrological and Water Resource Bureau,rümqi Xinjiang 830000,China;2.Bortala Hydrological and Water ResourceBureau,Bole Xinjiang 833400,China;3.Hami Hydrological and Water Resource Bureau,Hami Xinjiang 839000,China)

【机构】 新疆水文水资源局新疆博尔塔拉水文水资源勘测局新疆哈密水文水资源勘测局 新疆乌鲁木齐830000新疆博乐833400新疆乌鲁木齐830000新疆哈密839000

【摘要】 艾比湖在中更新世为鼎盛期,湖面积曾达3 000 km2,贮水量700×108m3,为良好的淡水湖.由于地壳运动和气候的暖干变化,湖面萎缩,到20世纪50年代初湖面积降至1 070 km2.自20世纪50年代以来,由于大规模的水土开发,灌区人口、灌溉面积和引水量大幅度增加,入湖水量急剧减少.从20世纪50年代至80年末,灌区人口增加了59.3×104人,灌区面积增加了16.43×104km2之多,净耗水量增加了8.13×108m3左右.湖面积一度降至499 km2(1987年),湖水矿化度达100 g.L-1左右.湖泊的萎缩,导致生态环境的劣变,表现为沙漠化程度加速,浮尘和沙暴天气增加,人畜受害,也导致野生动物的数量减少.20世纪80年代后,由于气候暖湿转型效应,降水和河川径流量有所增加.尤其是大力推广先进节水灌溉技术和退耕还林以及培育生态林等措施,使得入湖水量大幅度增加,特别是2001—2005年的5 a间,年均入湖水量达7.7×108m3,比1989年增加了76%,湖水面积维持在800~950 km2左右.目前生态环境已有所恢复和改观,荒漠植被得到一定程度的修复,沙尘天气明显减少,已有野生动物出没其间.

【Abstract】 The Ebinur Lake(44°30′N,82°25′E) at the north piedmont of west Tianshan Mountains is characterized by its wide area and shallow depth,thus its area change is extremely sensitive to the climate change. Ebinur Lake was a great well freshwater lake with an area of 3000 km~2 and a volume of 700×10~8 m~3 in the middle Pleistocene period.Because of tectonically movement of the Earth and warm-dry climate change,the lake area shrank to 1070 km~2 at the beginning of 1950s.The inflow runoff to Ebinur Lake decreased sharply as large increase of water consumption since 1950s,because of large-scale water and soil development,the increase of population and irrigation area in the watershed.From 1950s to the late of 1980s,the population had increased by 59.3× 10~4,the irrigation area increased by 16.43×10~4 km~2,net consumed water increased by 8.13×10~8m~3,and result in the lake area was reduced to 499 km~2 and the water salinity reached about 100 g·L~-1 in 1987.The shrinking of the lake would result in eco-environmental deterioration: accelerated the extent of desertification,floating dust and sandstorm increasing;the number of wild animals decreasing.After 1987,the increasing of precipitation and river runoff as climate change from warm-dry pattern to warm-wet pattern,and using measurements of water-saving irrigation technology and the development of ecological forests and returning farmland to forest,the inflow runoff to the lake increased rapidly,and the lake area was enlarged to 1096 km~2 in May 2000,to restore to about the water level in 1957.Especially in years of 2001-2005,the mean annual runoff of inflowing into Ebinur Lake reached 7.7×10~8m~3,increased by 76% than 1989,and the lake water kept in an area of 800-950 km~2.The ecological environment has been restored and improved,the desert vegetation has been partly restoration,dust weather has significantly decreased,and wildlife animals have appeared there.

【关键词】 艾比湖湖面变化气候变化生态环境
【Key words】 Ebinur Lakelake areaclimate changeeco-environment
【基金】 中国科学院寒区旱区环境与工程研究所前沿领域创新项目(2004117);中国沙漠气象科学研究基金项目(sqj-2005002)资助
  • 【文献出处】 冰川冻土 ,Journal of Glaciology and Geocryology , 编辑部邮箱 ,2006年06期
  • 【分类号】X820.3;P343.3
  • 【被引频次】27
  • 【下载频次】457
节点文献中: 

本文链接的文献网络图示:

本文的引文网络