干旱区生态环境知识资源中心(Arid): 2002年塔里木河流域四条源流区间耗水分析

Arid

	2002年塔里木河流域四条源流区间耗水分析
其他题名	Interzone Water Consumption from Four Source Streams to Mainstream of Tarim River, Xinjiang, in 2002
	王顺德 1; 李红德 1; 胡林金 2; 苏宏超 3; 曹晓莉 1; 孙本国 2; 李春梅 1; 毛炜峄 4; 王进 1
来源期刊	冰川冻土
ISSN	1000-0240
出版年	2004
卷号	26 期号:4 页码:496-502
中文摘要	2002年塔里木河四条源流出山口天然径流量273.9108m3, 比多年平均值多46.9108m3, 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219.1108m3, 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65.90108m3, 占出山口天然径流量的60%; 叶尔羌河流域耗水量61.92108m3, 年内无水量进入塔里木河干流; 和田河流域耗水量36.45108m3, 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%.
英文摘要	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 manmade transfer channel. There are numerous other rivers coming down from the mountains that disap-pear 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 10s ms from four mountains basins of Aksu, Hotan, Yarkant and Kaidu-Konque Rivers drain into the Tarim basin, more 46. 9 108m3than 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 10s m3 for Aksu, 60% of annual virgin flow; 61. 92 10~8 m~3 for Yarkant, no water drain into the mainstream of Tarim River; 36. 45 * 10~8m~3 for Hotan, 80. 9% of annual virgin flow; 54. 76 * 10~8 m~3 for the Kaidui - Kongque, 95. 9% of annual virgin flow.
中文关键词	塔里木河 ; 源流 ; 区间耗水 ; 2002年
英文关键词	Tarim Rive basin source stream interzone water consumption 2002
语种	中文
国家	中国
收录类别	CSCD
WOS类目	GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向	Geology
CSCD记录号	CSCD:1688938
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/204798
作者单位	1.阿克苏水文水资源勘测局, 阿克苏, 新疆 843000, 中国; 2.喀什水文水资源勘测局, 喀什, 新疆 844000, 中国; 3.新疆维吾尔自治区水文水资源局, 乌鲁木齐, 新疆 830000, 中国; 4.新疆环境气象中心, 乌鲁木齐, 新疆 830002, 中国
推荐引用方式 GB/T 7714	王顺德,李红德,胡林金,等. 2002年塔里木河流域四条源流区间耗水分析[J],2004,26(4):496-502.
APA	王顺德.,李红德.,胡林金.,苏宏超.,曹晓莉.,...&王进.(2004).2002年塔里木河流域四条源流区间耗水分析.冰川冻土,26(4),496-502.
MLA	王顺德,et al."2002年塔里木河流域四条源流区间耗水分析".冰川冻土 26.4(2004):496-502.