干旱区生态环境知识资源中心(Arid): 塔里木河流域2004年"四源一干"河川径流情势及输水运行分析

Arid

	塔里木河流域2004年"四源一干"河川径流情势及输水运行分析
其他题名	Streamflow Regime of Four Source Rivers and Mainstream of Tarim River,Xinjiang and Transfer Water Course in 2004
	阿迪力·艾则孜 1; 王建文 2; 张建岗 3; 毛炜峄 4; 张丽萍 5; 沈永平 6; 王顺德 1; 王刚 3
ISSN	1000-0240
出版年	2006
卷号	28 期号:6 页码:931-940
中文摘要	2004年塔里木河流域平原的年平均气温特高,山区偏高.平原与山区年降水量均正常略偏多,流域内春夏季0 ℃层高度偏低.2004年塔里木河四条源流出山口天然径流量224.010~8m~3,属平水年.天山南坡的河流水量偏丰,阿克苏河偏多15.9%,为丰水年;开都河-孔雀河偏多4.2%,为平略偏丰水年.而喀喇昆仑山及昆仑山北坡的河流水量均少于多年均值,如叶尔羌河偏少10.8%,为偏枯水年;和田河偏少17.9%,为枯水年.四条源流阿克苏河、和田河、叶尔羌河、开都河-孔雀河入塔里木河总水量为27.0210~8m~3,占四条源流出山口天然径流总量的12.1%,叶尔羌河全年无水输入塔里木河.2004年塔里木河干流上游段阿拉尔-英巴扎耗水量为19.1910~8m~3,是干流最大的耗水区段;中游段英巴扎-恰拉耗水量为7.53010~8m~3,为治理前的30.3%,是输水堤工程竣工和加强管理的效益.2004年4月22日至6月25日,实施了第6次从博斯腾湖向塔里木河下游应急输水,历时65 d从博斯腾湖调出水量1.60010~8m~3,大西海子水库泄洪闸向下游输水量 1.02010~8m~3,水头再次到达台特玛湖,多年来的调水已使下游河段两岸生态环境有了明显改善.
英文摘要	Basin is the biggest arid inland basin in China. The Aksu, Hotan, Yarkant and Kaidu-Konque Rivers are four source rivers of Tarim River drainage. The three tributary river systems (Aksu, Hotan and Yarkant) that contribute flows to the Tarim River join just above the Aler gauging station where the Tarim River begins. From the confluence of its three main contributing tributaries, the Tarim River mainstream extends 1 321 km to Taitema Lake. 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. The annual mean air temperature was unusual high in plain, but was slight higher in mountain regions in Tarim River Basin in 2004. Both precipitations in plain and mountains were a little more than normal. The 0℃ level height was lower in spring and summer in Tarim River Basin. In 2004 , total annual virgin flow of 224.0l0~8m~3 from four mountains basins of Aksu, Hotani Yarkant and Kaidu-Konque Rivers drain into the Tarim basin, is an normal hydrological year. The Aksu River and Kaidu-Konque Rivers from the south slope of Tianshan Mountains have a large runoff rising comparing with average annual runoff, Aksu River, increasing by 15. 9%, was an a-bundant hydrological year; Kaidu-Konque Rivers, increasing by 4.2% , was a slight abundant hydro-logical year. But the runoff in Yarkant River from the Karakorum and Hotan River from the West Kunlun Mountains were less than average annual runoff, Yarkant River, decreasing by 10. 8%, was a little shortage of water years Hotan River, decreasing by 17.9%, was a shortage of water year. The total discharge of the four source rivers, which are Aksu, Hotan, Yarkant and Kaidu-Konque Rivers, drain into Tarim River is 27.0210~8m~3 in 2004, occupy up 12.1% of annual virgin flow from mountains basin. The Yarkant River is the only river no water drain into the mainstream of Tarim Rive. The interzone consumed water of the Tarim River mainstream are estimated to be 19.19 * 10~8m~3 for the upper course from Aler to Yingbazha, the largest consumed section of the Tarim River mainstream; 7.530* 10~8m~3 for the middle course from Yingbazha to Qiala, occupy up 30.3 % of the consumption that before harness. The proportion of consumed water of upper, middle and downstream occupy the whole consumed water of Tarim River mainstream comparing with their own woodland proportion respectively, the proportion of consumed water was more in the upper stream course, was a little in the middle streams course, and was correspond in the lower course. During April 22 to June 25, 2004, the sixth ecological emergency water diversion project was carried out in the lower reaches of Tarim River, transfer water 1. 60010~8m~3 from Bosten Lake, outflow 1.02010~8m3 drains into Taitema Lake, from Daxihaizi Reservoir, and water reached in Taitema Lake again in 2004.
中文关键词	2004年 ; 塔里木河 ; 河川径流 ; 输水运行 ; 耗水 ; 生态需水
英文关键词	2004 Tarim River runoff water diversion consumed water ecological water demand
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:2637149
来源机构	中国科学院西北生态环境资源研究院
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/219451
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.巴州水文水源勘测局, 库尔勒, 新疆 841000, 中国; 3.塔里木河流域管理局, 库尔勒, 新疆 841000, 中国; 4.新疆气候中心, 乌鲁木齐, 新疆 830002, 中国; 5.博尔塔拉水文水资源勘测局, 博乐, 新疆 833400, 中国; 6.中国科学院寒区旱区环境与工程研究所, 兰州, 甘肃 730000, 中国
推荐引用方式 GB/T 7714	阿迪力·艾则孜,王建文,张建岗,等. 塔里木河流域2004年"四源一干"河川径流情势及输水运行分析[J]. 中国科学院西北生态环境资源研究院,2006,28(6):931-940.
APA	阿迪力·艾则孜.,王建文.,张建岗.,毛炜峄.,张丽萍.,...&王刚.(2006).塔里木河流域2004年"四源一干"河川径流情势及输水运行分析.,28(6),931-940.
MLA	阿迪力·艾则孜,et al."塔里木河流域2004年"四源一干"河川径流情势及输水运行分析".28.6(2006):931-940.