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晋西黄土残塬区坡面的日蒸散模型
引用本文:胡振华,王治国.晋西黄土残塬区坡面的日蒸散模型[J].中国水土保持科学,2003,1(1):95-98.
作者姓名:胡振华  王治国
作者单位:1. 山西农业大学林学院,030801,山西,太谷
2. 水利部水利水电规划设计总院,100011,北京
基金项目:国家"九五"科技攻关项目"晋西残塬区高产农业综合发展研究"(96-004-05-06)
摘    要: 基于蒸发的物理机制,分析晋西黄土残塬区影响坡面蒸发的主导因子,提出了可以在不饱和土壤水分情况下应用的坡面土壤蒸发模型。认为坡度、坡向、土壤含水量、最高气温及植被盖度是影响坡面蒸发的主导因子。该模型对精确定量黄土残塬区小流域的生态需水及指导小流域水土保持生态环境建设具有重要意义。

关 键 词:黄土残塬区  坡面  日蒸散模型
修稿时间:2003年3月28日

Daily Evaportranspiration Models for Slopes of Loess Gully Area in Western Shanxi Province
Hu Zhenhua,Wang Zhiguo.Daily Evaportranspiration Models for Slopes of Loess Gully Area in Western Shanxi Province[J].Science of Soil and Water Conservation,2003,1(1):95-98.
Authors:Hu Zhenhua  Wang Zhiguo
Institution:1.Forestry College of Shanxi Agricultural University, 030801, Taigu , Shanxi, China;2.Water Resources and Hydropower Planning and Design General Institute Ministry of Water Resource, 100011, Beijing, China
Abstract:Based on the physical mechanism of evaportranspiration, this paper analyzed main factors affecting slope e-vaportranspiration in loess gully area of Western Shanxi province; put forward evaportranspiration models of slope soil in the condition of unsaturated soil moisture. It is shown that the slope gradient, aspect, soil moisture, maximum temperature , vegetation coverage are the major factors affecting slope evaportranspiration. The models may be used well in precise computing ecological water requirement and guiding of soil and water conservation in small watershed.
Keywords:loess gully area  slope  daily evaportranspiration models
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