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蒸散发条件下农田土壤水盐动态简化模型
引用本文:张妙仙,毛任钊.蒸散发条件下农田土壤水盐动态简化模型[J].中国生态农业学报,2003,11(3):102-105.
作者姓名:张妙仙  毛任钊
作者单位:中国科学院石家庄农业现代化研究所,石家庄,050021
基金项目:国家重点基础研究(973)发展规划项目(G1999011803)和中国科学院知识创新工程项目(KZCX-SW-317-01,KZCX2-405)共同资助
摘    要:利用需水系数、蒸腾系数和潜水蒸发经验公式,引入水分迁移系数和盐分迁移系数,建立了蒸散发条件下农田土壤水盐动态简化模型。提出作物根系吸水比例系数,用以区分计算土层下边界的根系吸水项和土壤毛管水上升项。引入盐分影响下的作物蒸散发修正系数,并与水盐生产函数相反馈进行土壤水盐动态的修正。该模型简单适用,可用于蒸散发期间田间水盐状况的调控管理。

关 键 词:蒸散发  根系吸水  水盐动态模型
收稿时间:2002/11/18 0:00:00
修稿时间:2002年11月18

The simplified model of salt-water regimes in farm land soil under the processing of evaportranspiration
ZHANG Miao- Xian and MAO Ren-Zhao.The simplified model of salt-water regimes in farm land soil under the processing of evaportranspiration[J].Chinese Journal of Eco-Agriculture,2003,11(3):102-105.
Authors:ZHANG Miao- Xian and MAO Ren-Zhao
Abstract:According to the principle of salt-water balance and the observation and experimental data about ground water, irrigation and salt regimes, making use of water-need coefficient and transpiration coefficient and introducing salt and water migration coefficients, this paper presents a simplified model of salt-water regimes of upper soil layer under the processing of evapotranspiration. Based on the growth function of the crop roots, a water uptake ratio coefficient of crop roots is presented also, so that divide the lower boundary water flow into root extraction and soil capillary water movement. Introduced salt modified coefficient to evapotranspiration and feedback with the salt and water production function, evapotranspiration and the salt-water regime model are modified. The model is simple and suitable for the regulation and control of water and salt regimes on farmland under the processing of evapotranspiration.
Keywords:Evaportranspiration  Crop root water uptake  Salt-water regime model
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