摘要
为探索干旱地区冻结滞水形成及融化规律, 经室内冻融模拟试验结果表明, 在冻结势作用下包气带水和空气中水分以液态和气态向冻结滞水层迁移富集, 含水率比冻结前增加11. 15% ~14. 75% , 主要富集在0~20 cm 的深度,形成倒置富水性在解冻期间由上向下融化,融水以蒸发为主消耗部分向下运动可见, 冻结滞水是干旱区林木等植物越冬春季繁衍不可缺少的水资源应用冻结滞水的理论和动态规律, 采用科学的技术措施, 提高其含水量和造林成活率及生长量,
The formation of frozen stagnant water and its thawing are studied in the arid areas Modelling experiment of freezing thawing shows that owing to frost water migrates into the freezing stagnant water layer from kremastic water and atmospheric water in terms of vapour and moisture It is found that water content increases 11 15%~14 75% after frost, mainly enriching at the depth of 0~0 2 m During the thawing period, the soil is thawing from the surface downwards, and the meltwater is mainly consumed with transpiration and partly percolates downwards The frozen stagnant water becomes an important water supply for plant growth and reproduction during winter and spring in the arid areas Applying the formation theory and the moving regulation of the frozen stagnant water, and taking scientific measures to increase this water content, afforestation survival rate and growth amount in order to restore vegetation and eco environment has obvious theoretical and social significance
出处
《冰川冻土》
CSCD
北大核心
1999年第3期269-272,共4页
Journal of Glaciology and Geocryology
基金
国家自然科学基金
关键词
干旱地区
冰结滞水
造林
冻土
arid area
frozen stagnant water
afforestation