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2002年塔里木河流域四条源流区间耗水分析

Interzone Water Consumption from Four Source Streams to Mainstream of Tarim River, Xinjiang, in 2002

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【作者】 王顺德李红德胡林金苏宏超曹晓莉孙本国李春梅毛炜峄王进

【Author】 WANG Shun-de~(1),LI Hong-de~(1),HU Lin-jin~(2),SU Hong-chao~(3), CAO Xiao-li~(1),SUN Ben-guo~(2), LI Chun-mei~(1),MAI We-iyi~(4), WANG Jin~(1) (1. Aksu Hydrological and Water Resource Bureau, Aksu Xinjiang 843000, China; 2.Kashgar Hydrological and Water Resource Bureau,KashgarXinjiang 844000 ,China; 3. Xinjiang Hydrological and Water Resource Bureau, rümqi Xinjiang 830000, China;4. Environmental Meteorology Centre of Xinjiang, rümqi Xinjiang 830002, China)

【机构】 阿克苏水文水资源勘测局喀什水文水资源勘测局新疆维吾尔自治区水文水资源局新疆环境气象中心阿克苏水文水资源勘测局 新疆阿克苏 843000新疆阿克苏 843000新疆喀什 844000新疆乌鲁木齐 830000新疆乌鲁木齐 830002新疆阿克苏 843000

【摘要】 2002年塔里木河四条源流出山口天然径流量273.9×108m3,比多年平均值多46.9×108m3,偏多20.7%,属丰水年.其中发源于天山山脉的阿克苏河和开都河 孔雀河径流增幅大,水量充沛,属丰水年,而发源于昆仑山脉的叶尔羌河和和田河径流量保持多年均值年.2002年度,四条源流区总耗水量219.1×108m3,占出山口天然径流量的80.0%.其中阿克苏河流域总耗水量为65.90×108m3,占出山口天然径流量的60%;叶尔羌河流域耗水量61.92×108m3,年内无水量进入塔里木河干流;和田河流域耗水量36.45×108m3,占出山口天然径流量的80.9%.开 孔河流域内耗水54.76×108m3,占出山口天然径流量的95.9%.

【Abstract】 The Tarim River Basin is surrounded by mountains on three sides and is a closed-basin with no outlet to the sea. From the confluence of its three main contributing tributaries, the Tarim River mainstream extends 1321 km to Taitema Lake. The three tributary river systems that contribute flows to the Tarim River (Aksu, Hotan and Yarkant) join just above the Aler gauging station where the Tarim River begins.In addition the Kaidu-Konque River Basin, which is hydrologically separate from the Tarim River, contributes water to the Tarim River by means of a man-made transfer channel. There are numerous other rivers coming down from the mountains that disappear into the desert. A number of rivers fed by snowmelt and glacier melt begin in the mountains and drain into the basin. In 2002, annual virgin flow of about 273.9 108m3from four mountains basins of Aksu, Hotan, Yarkant and Kaidu-Konque Rivers drain into the Tarim basin, more46.9 108m3 than average annual streamflow, excessive more 20.7% . The Aksu River and Konque-Kaidu Rivers from Tianshan Mountains have a large runoff rising comparing with average annual runoff, and keep normal runoff in Yarkant River from the Karakorum and Hotan River from the West Kunlun Mountains. Most of this water is consumptively used before reaching the confluence, total consumptive water of four source streams sum up 219.1 108m3, occupy up 80% of annual virgin flow from mountains basin. Actual annual consumptive water were measured to be 65.90 108m3for Aksu, 60% of annual virgin flow; 61.92 108m3for Yarkant,no water drain into the mainstream of Tarim River; 36.45×108m3for Hotan, 80.9% of annual virgin flow; 54.76×108m3for the Kaidui-Kongque, 95.9% of annual virgin flow.

【关键词】 塔里木河源流区间耗水2002年
【Key words】 Tarim Rive basinsource streaminterzone water consumption2002
【基金】 国家自然科学基金项目(40371026;90202013)资助
  • 【文献出处】 冰川冻土 ,Journal of Glaciology and Geocryology , 编辑部邮箱 ,2004年04期
  • 【分类号】P333
  • 【被引频次】36
  • 【下载频次】216
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