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内蒙古西部黄土丘陵区土壤水分动态初探
引用本文:寇志强,王其昌.内蒙古西部黄土丘陵区土壤水分动态初探[J].水土保持通报,1992,12(6):60-63,77.
作者姓名:寇志强  王其昌
作者单位:内蒙古自治区水利科学研究所 呼和浩特市 010020;内蒙古自治区水利科学研究所 呼和浩特市 010020
摘    要:通过对内蒙古西部黄土丘陵区土壤水分的初步研究,表明:该区土壤水分的垂直动态分布分为三个不同层次,即:水分不稳定层(0~40cm);中间过渡层(40~100cm);水分相对稳定层(100~200cm);旱作土壤水分的动态变化与降雨的变化基本一致;作物对土壤水分的消耗主要是当年降雨。

关 键 词:土壤水分动态  土壤含水量
收稿时间:1992/4/27 0:00:00

A Discussion on Soil Moisture Dynamics in Loess Hilly Areas of the West Inner Mongolia
Kou Zhiqang and Wang Qichang.A Discussion on Soil Moisture Dynamics in Loess Hilly Areas of the West Inner Mongolia[J].Bulletin of Soil and Water Conservation,1992,12(6):60-63,77.
Authors:Kou Zhiqang and Wang Qichang
Institution:Institute of Water Conservancy Science of Inter Mongolia, Hohhot, Inner Mongolia, 010020;Institute of Water Conservancy Science of Inter Mongolia, Hohhot, Inner Mongolia, 010020
Abstract:Through the preliminary study of soil moisture in loess hilly areas of the West Inner Mongo-lia, it was concluded that the dynamic distribution of soil moisture in vertical direction can be di-vided into three section, i. e., the fluctuation section (0 - 40cm), the middle transformation section(40- 100cm), the relative stable section (100 - 200cm). There is agreement between the dynamicchanges in soil moisture and the changes in rainfall in arid farmland.
Keywords:loess hilly areas  soil moisture dynamics  vertical distribution
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