地下排水和渗灌条件下麦田土壤水分变化模拟  

Simulation of Soil Moisture Fluctuation in Winter Wheat Fields under Subdrainage and Seepage Irrigation

作　　者：朱成立[1] 邵孝侯[1] J.D.Owusu 

机构地区：[1]河海大学水利水电工程学院,江苏南京210098

出　　处：《河海大学学报（自然科学版）》2000年第2期23-26,共4页Journal of Hohai University(Natural Sciences)

基　　金：江苏省水利动力工程重点开放实验室基金资助项目!(K9874);中国博士后基金资助项目! (中国博士后基金委员会 [1998]6号文);国家"九

摘　　要：用Feddes模型模拟了地下排水和渗灌条件下麦田表层土壤的水分动态变化过程 .结果表明 :该模型能敏感地预测渗灌和排降后农田表层土壤的水分动态 。Numerical simulation of surface soil moisture status in winter wheat fields under subdrainage and seepage irrigation is conducted based on the Feddes model.The results show that the model could predict surface soil moisture dynamic fluctuation in the fields after seepage irrigation and subdrainage.Soil moisture of root accumulating layers obtained by the model could be used to guide irrigation and subdrainage for winter wheats in the North Huai River area of Jiangsu province.

关 键 词：地下排水 渗灌 土壤水分 麦田 

分 类 号：S152.7[农业科学—土壤学] S275[农业科学—农业基础科学]