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北京典型地区灌溉条件下包气带水分运移特征研究

刘颖超 邢国章 刘凯 谢振华

城市地质Issue(1):20-24,66,6.
城市地质Issue(1):20-24,66,6.

北京典型地区灌溉条件下包气带水分运移特征研究

Research on the Characteristics of Water Movement under Irrigation Condition in Vadose Zone in the Typical Area of Beijing

刘颖超 1邢国章 2刘凯 1谢振华1

作者信息

  • 1. 北京市水文地质工程地质大队,北京 100195
  • 2. 北京市地质工程勘察院,北京 100048
  • 折叠

摘要

Abstract

Base on the irrigation experiment of moisture and salt content migration of the vadose zones in-situ in the Zhangjiawan area, the paper analyzes the migration characteristics of moisture movement of unsaturated zones from the view of moisture energy. It shows that moisture migration of vadose zones can be roughly divided into three zones and the process of groundwater recharge under irrigation, the deep of the moisture migration. The ground water level rises very low under the condition of irrigation and the irrigation recharge quantity was very little, which was calculated by unsaturated lfow Darcy's law.

关键词

包气带/含水量/土水势/水分运移/补给量

Key words

Vadose zone/Water content/Soil water potential/Moisture movement/Recharge quantity

分类

天文与地球科学

引用本文复制引用

刘颖超,邢国章,刘凯,谢振华..北京典型地区灌溉条件下包气带水分运移特征研究[J].城市地质,2015,(1):20-24,66,6.

城市地质

2097-3764

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