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半湿润地区植被影响下的沙地水分动态
引用本文:冯起,高前兆.半湿润地区植被影响下的沙地水分动态[J].干旱区研究,1994,11(4):58-63.
作者姓名:冯起  高前兆
作者单位:中国科学院兰州沙漠研究所
摘    要:半湿润地区沙地在植被作用下土壤水分动态随季节变化,可以划分为春,夏,秋,冬四个阶段。随土层深度而增加可划分出几个明显层次:浅耕层,根系作用下水分极活跃变化层,地下水持续影响层。由于不同植物生长季不同,植物发育状况不同,生长所处位置不同而呈现出特写的土壤水分变化形势。降水,土壤性质,地下水强烈地影响着本沙地土壤水分的动态变化。植物根系对土不分动态变化影响明显,植被覆盖下的半湿润沙地表层干沙层发育最大

关 键 词:植被  半湿润地区  沙地  水分动态

Study Soil Water Variability of Sandy Land influencing by Vegetation in the Semi-humid Zone
Feng Qi,Gao.Qianzhao,Zhang Xiaoyou.Study Soil Water Variability of Sandy Land influencing by Vegetation in the Semi-humid Zone[J].Arid Zone Research,1994,11(4):58-63.
Authors:Feng Qi  GaoQianzhao  Zhang Xiaoyou
Abstract:Semi-humid varibility of sand-larnd water influencing by vegetation can be divided Spring,Summer,Autumn,Winter four phrases with the seasons change. From the top to the bottom of a retrical profile there exist four clearly distinctive layers of soil water:shallow ploughing layer, active layer influencing by root system, stable layer influencing by groud water. Different vegetation show speoally soil water variation development according geographical position. Precipitation, soil characteristic ground water intense influence the trends change of soil water. Root system of vegetation clearly influence the trends change of soil water. Semi-humid sandy-land dry sand layer depth can reach 4-5cm.
Keywords:Soil-variability  Sandy-land  influencing by vegetation  the semi-humide zone    
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