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冻结期和冻融期土壤水分运移特征分析
引用本文:郭占荣,荆恩春,聂振龙,焦鹏程,董华.冻结期和冻融期土壤水分运移特征分析[J].水科学进展,2002,13(3):298-302.
作者姓名:郭占荣  荆恩春  聂振龙  焦鹏程  董华
作者单位:中国地质科学院水文地质环境地质研究所, 河北, 石家庄, 050061
基金项目:"九五"国家重点科技攻关项目(96-912-01-03S)资助
摘    要:西北内陆盆地冻结期和冻融期几乎占全年时间的1/2,该时期土壤水分运移特点与非冻结期存在较大差异.本文根据北疆昌吉平原区土壤水分运移观测试验,分析了冻结期和冻融期土壤水势分布和土壤含水量变化规律及其与潜水的转化关系,并阐述了冻融水的生态环境意义.

关 键 词:土壤水势能    土壤含水量    冻结期    冻融期    内陆盆地    西北
文章编号:1001-6791(2002)03-298-05
收稿时间:2001-04-09
修稿时间:2001年4月9日

Analysis on the characteristics of soil moisture transfer during freezing and thawing period
GUO Zhan-rong,JING En-chun,NIE Zhen-long,JIAO Peng-cheng,DONG Hua.Analysis on the characteristics of soil moisture transfer during freezing and thawing period[J].Advances in Water Science,2002,13(3):298-302.
Authors:GUO Zhan-rong  JING En-chun  NIE Zhen-long  JIAO Peng-cheng  DONG Hua
Affiliation:Institute of Hydrology and Environmental Geology, CAGS, Shijiazhuan 050061, China
Abstract:The duration of freezing and thawing period almost accounts for a half year in the inland basin of northwestern China,in which the characteristics of soil moisture transfer is greatly differential from that of non-freezing period.Based on the observatory experiment on soil moisture transfer in inland plains,the distribution of soil moisture potential and the regularity of soil moisture ratio variation as well as its converting to groundwater during freezing and thawing period are analyzed.The significance of thawed water in eco-environment is also expounded.
Keywords:soil moisture potential  soil moisture ratio  freezing period  thawing period  inland basin  northwestern China  
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