收藏设为首页 广告服务联系我们在线留言

干旱区地理 ›› 2001, Vol. 24 ›› Issue (1): 62-66.doi: 10.13826/j.cnki.cn65-1103/x.2001.01.011

• • 上一篇    下一篇

渭干河灌区参考作物潜在腾发量的计算及相关分析

胡顺军1, 艾尼瓦尔·吾买尔2, 宋郁东1, 周宏飞1, 田长彦1, 王永平2, 蒋庆华2, 艾则孜2, 黄文山2, 吐尔逊2   

  1. 1.中国科学院新疆生态与地理研究所, 乌鲁木齐 830011;
    2.渭干河流域管理处, 库车 842000
  • 收稿日期:2000-04-28 修回日期:2001-01-18 发布日期:2025-12-31
  • 基金资助:
    国家重点基础研究973项目 (编号:G1999043506)和“西部之光”项目

CALCULATION AND DEPENDENCE ANALYSIS FOR REFERENCE CROP EVAPOTRANSPIRATION IN WEIGAN RIVER IRRIGATED AREA

HU Shunjun1, Ainiwaer UMAIER2, SONG Yudong1, ZHOU Hongfei1, TIAN Changyan1, WANG Yongping2, JIANG Qinghua2, Aizezi2, HUANG Wengshan2, Tuersun2   

  1. 1. Xinjiang Institute of Ecology and Geography, CAS, Urumqi 830011;
    2. Weigan River Management Bureau, K uche county, 842000
  • Received:2000-04-28 Revised:2001-01-18 Online:2025-12-31

摘要: 利用Penman公式, 根据位于渭干河灌区内的库车、沙雅、新和三县气象站1992~1996年气象观测资料, 计算了参考作物潜在腾发量并建立了参考作物潜在蒸发量与其它气象要素的经验关系。根据这些经验关系进行参考作物潜在腾发量的估算, 其结果可供该地区作物耗水量等研究时参照使用。

关键词: 渭干河灌区, 参考作物潜在蒸发量, Penman公式, 气温, 水面蒸发, 饱和差

Abstract: Based on monthly meteorological data from 1992 to 1996 of Kuche, Shaya, Xinhe meteorological Stations in Weigan river basin, monthly reference crop evapotranspiration is calculated by Penman (FAO) Equation. Characteristics of reference crop evapotranspiration are analyzed. Meanwhile, empirical relationship between reference crop evapotranspiration and other meteorological factors are established. The results show that (1) In the unfreezing period the average daily reference crop evapotranspiration are 3.78~4.13 mm/d, 3.63~3.87 mm/ d, 3.43~3.97 mm/d in Kuche, Shaya, Xinhe county respectively; The annual variation is not great. (2) The maximum of reference crop evapotranspiration occurs in June or July, which is about 5.32~6.17 mm/d. The minimum of that occurs in October, which is about 0.89~1.45 mm/d. Monthly variation is great. (3) In March or April or October, aerodynamic term is greater, the wind speed is the main factor affecting the reference crop evapotranspiration; in May to September radiation term is greater, the radiation is the main factor affecting the reference crop evapotranspiration. (4) The relationship between monthly reference crop evapotranspiration and monthly average air temperature is linear during monthly average air temperature raises, and is exponential during monthly average air temperature drops. (5) The relationship between reference crop evapotranspiration and water surface evaporation is linear, its proportion coefficient is about 0.54. (6) The relationship between reference crop evapotranspiration and saturation deficiency is linear during monthly average air temperature drops, and is logarithmic during monthly average air temperature raises. (7) Empirical relationship between reference crop evapotranspiration and air temperature and that between reference crop evapotranspiration and 20 cm pan evaporation and that between reference crop evapotranspiration and saturation deficiency can be used in the estimation of reference crop evapotranspiration in a simple way with preferable accuracy. The results can also be used for the study of crop water consumption in this distract.

Key words: Weigan river irrigated area, reference crop evapotranspiration, Penman(FAO) equation, water surface evaporation, air temperature, saturation deficiency

中图分类号: 

  • S161.42