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干旱区地理 ›› 2000, Vol. 23 ›› Issue (1): 67-71.doi: 10.13826/j.cnki.cn65-1103/x.2000.01.012

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渭干河灌区陆面蒸发量估算

胡顺军1, 田长彦1, 周宏飞1, 李慧2   

  1. 1.中国科学院新疆生态与地理研究所, 乌鲁木齐 830011;
    2.新疆阿克苏市水电局, 阿克苏 843000
  • 收稿日期:1999-03-05 修回日期:1999-10-12 发布日期:2025-12-31

ESTIMATION OF LAND EVAPORATION IN THE WEIGAN IRRIGATED AREA, XINJIANG

Hu Shunjun1, Tian Changyan1, Zhou Hongfei1, Li Hui2   

  1. 1. Xinjiang Institute of Ecology & Geography, Chinese Academy of Science, Urumqi, 830011, China;
    2. Aksu Water Conserv ancy Bureau, Aksu 843000, China
  • Received:1999-03-05 Revised:1999-10-12 Online:2025-12-31

摘要: 根据渭干河灌区实测资料, 采用水量平衡法、水热平衡法、Turk经验公式和折算系数法对监测区的陆面蒸发量进行了估算, 分析了各估算方法的精度。结果表明:在内陆干旱绿洲灌区内, 陆面蒸发量高出降水量几十倍, 陆面蒸发是其水资源的主要消耗;水量平衡法、水热平衡法和折算系数法适用于干旱区陆面蒸发量的估算。

关键词: 渭干河, 灌区, 陆面蒸发量, 估算

Abstract: The Weigan irrigated is located in an alluvia-l diluvial plain in the northern part of Tarim Basin, and its elevation varies in a range of 920~1, 100 m a. s. l. Climate here is extremely dry, the annual precipitation is only 51.6 mm, the annual evaporation from water surface, however, varies in a range of 1992.0~2863.4 mm. It is rich in sunshine and solar heat resources, the annual temperature changes in a range of 10.5~11.4℃, and light soil and sandy soil are the main soil types in the irrigated area. Weigan River is its only irrigation water source, and land evaporation is the main water consumption. Currently there are many methods for calculating land evaporation, however, the parameters needing in some calculating methods are difficult to determine. In this paper, land evaporation in the Weigan irrigated area (4, 130.3 km2) is estimated by using water budget method, Turk empirical formula, and reduction coefficient method based on the available data. The results are as follows:
(1) In the Wergan irrigated area, the annual land evaporation is 576 mm, it is 8. 7 times higher than the annual precipitation (67 mm), which is one of the results of human activities, such as water diverting for irrigation.
(2) The evaporation mechanism in the irrigated areas in arid regions is mainly conrolled by water supply conditions, and land evaporation is the main consumption of water resources in arid regions. Land evaporation occupies 89. 4% of the total water loss in the Weigan irrigated area, of which 99% are surface water.
(3) Land evaporation estimated by water budget method is reliable and can be regarded as the standard to calibrate the precision of that estimated by other methods. The relative error of land evaporation estimated by water-heat budget method varies in a range of 4%~10%. The empirical formula used for estimating land evaporation with reduction coefficient method is as :E-0.30 E 20, the reduction coefficient is 0.30, and the comprehensive coefficient of land evaporation is 0.49. These show that land evaporation in the oasis irrigated areas in arid regions can be estimated by water-heat budget method and can also be calculated by evaporation from water surface.

Key words: Weigan River, irrigated area, land evaporation, estimation

中图分类号: 

  • S161.4