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低定额灌溉条件下农田土壤水蒸散模型的研究
引用本文:韩雄,张强,安静华.低定额灌溉条件下农田土壤水蒸散模型的研究[J].华北水利水电学院学报,2000,21(1):20-23.
作者姓名:韩雄  张强  安静华
作者单位:1. 山西省农科院土壤肥料研究所,山西,太原,030031
2. 水利部山西水利水电勘测设计研究院,山西,太原,030031
摘    要:在低定额灌溉条件下 ,农田土壤水分常处在水分胁迫条件下 ,对水分胁迫下农田土壤水分蒸散模型进行了研究 ,在水分胁迫下实际蒸散量 (ET)与潜在蒸散量 (ETm)之间关系为 :ET =KW·ETm·KW,与根层土壤有效水含量具有直线相关性 .模型中考虑根系分布的影响 ,能明显提高模型精度 ,为低定额灌溉确定农田实际耗水量提供科学依据 ,并提高农田土壤水分利用率

关 键 词:低定额灌溉  蒸散模型
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Study on evapotranspiration model of agricultural soil water under low irrigation
HAN Xong,ZHANG Qiang,AN Jing-hua.Study on evapotranspiration model of agricultural soil water under low irrigation[J].Journal of North China Institute of Water Conservancy and Hydroelectric Power,2000,21(1):20-23.
Authors:HAN Xong  ZHANG Qiang  AN Jing-hua
Abstract:Under low irrigation, agricultural soil water is usually stressed by water.A soil evapotranspiration modelwas studied under water stress.Under water stress, the relationship between actual evapotranspiration(ET) and potential evapotranspiration(ET m ) could be caculated as : ET= K w ET m , K w is linearly correlated with soil effective moisture. In this model, root distribution was considered, so the model precision was significantly improved. As a result,it could confirm actual water requirement so as to improve soil water efficiency.WX(5KG0,41]
Keywords:low irrigation  evapotranspiration  model  water stress
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