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蒸散发条件下农田土壤水盐动态简化模型 被引量:2
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作者 张妙仙 毛任钊 《中国生态农业学报》 CAS CSCD 2003年第3期102-105,共4页
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... 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。 展开更多
关键词 农田土壤水动态简化模型 蒸散发 需水系数 蒸腾系数 潜水蒸发经验公式 水分迁移系数 分迁移系数
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Saline Water Irrigation Scheduling Through a Crop-Water-Salinity Production Function and a Soil-Water-Salinity Dynamic Model 被引量:16
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作者 WANG Yang-Ren KANG Shao-Zhong +2 位作者 LI Fu-Sheng ZHANG Lu ZHANG Jian-Hua 《Pedosphere》 SCIE CAS CSCD 2007年第3期303-317,共15页
Using a crop-water-salinity production function and a soil-water-salinity dynamic model, optimal irrigation scheduling was developed to maximize net return per irrigated area. Plot and field experiments were used to o... Using a crop-water-salinity production function and a soil-water-salinity dynamic model, optimal irrigation scheduling was developed to maximize net return per irrigated area. Plot and field experiments were used to obtain the crop water sensitivity index, the salinity sensitivity index, and other parameters. Using data collected during 35 years to calculate the 10-day mean precipitation and evaporation, the variation in soil salinity concentrations and in the yields of winter wheat and cotton were simulated for 49 irrigation scheduling that were combined from 7 irrigation schemes over 3 irrigation dates and 7 salinity concentrations of saline irrigation water (fresh water and 6 levels of saline water). Comparison of predicted results with irrigation data obtained from a large area of the field showed that the model was valid and reliable. Based on the analysis of the investment cost of the irrigation that employed deep tube wells or shallow tube wells, a saline water irrigation schedule and a corresponding strategy for groundwater development and utilization were proposed. For wheat or cotton, if the salinity concentration was higher than 7.0 g L-1 in groundwater, irrigation was needed with only fresh water; if about 5.0 g L-1, irrigation was required twice with fresh water and once with saline water; and if not higher than 3.0 g L-1, irrigation could be solely with saline water. 展开更多
关键词 crop-water-salinity production function irrigation scheduling saline water irrigation water-salinity dy- namic model
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