利用Hydrus-1D模拟分层土壤剖面的水流运动
Hydrus-1D Modeling Water Flow Transport in a Layered Soil Profile
董晓华 1刘潇钧 2彭涛 1姚着喜 2郭梁锋 2刘璇璇2
作者信息
- 1. 三峡大学水利与环境学院,湖北宜昌443002;水资源安全保障湖北省协同创新中心,湖北武汉430072
- 2. 三峡大学水利与环境学院,湖北宜昌443002
- 折叠
摘要
[目的]研究分层土壤水分运移规律,进行水分运移的数值模拟.[方法]利用Hydrus-1D软件,通过设定不同上下边界条件,进行分层土壤的水分运移模拟.[结果]利用Hydrus-1D软件可以模拟到水分运移中观测点的水头、含水量及土壤上表层流量的随时间的变化规律.[结论]水分运移中的地面边界流量、水头和含水量与降雨量的变化直接相关,科学可靠的气象数据对水分运移的模拟非常重要.
Abstract
[Objective] The aim was to study the law of soil moisture movement and conduct numerical simulation.[Method] Using Hydrus-1D software,by setting different upper and lower boundary conditions,soil movement in a layered soil was simulated.[Result] The variation law of water head,moisture content and soil upper surface flow with time was simulated by using Hydrus-lD software.[Conclusion] Surface boundary flux,water head and water content are directly related to the change of rainfall.Scientific and reliable meteorological data is very important for the simulation of water movement.
关键词
Hydrus-1D/水分运移/数值模拟Key words
Hydrus-1D/Water flow/Numerical modeling引用本文复制引用
基金项目
水利部“十二五”公益性行业专项(201301066)
出版年
2016
国家科技期刊平台
NSTL
维普
万方数据