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流动沙丘干沙层厚度对土壤水分蒸发的影响
引用本文:刘新平,张铜会,赵哈林,何玉惠,云建英,李玉强.流动沙丘干沙层厚度对土壤水分蒸发的影响[J].干旱区地理,2006,29(4):523-526.
作者姓名:刘新平  张铜会  赵哈林  何玉惠  云建英  李玉强
作者单位:中国科学院寒区旱区环境与工程研究所,奈曼沙漠化研究站,甘肃,兰州,730000
基金项目:国家自然科学基金 , 中国科学院科研项目
摘    要:利用Micro-lysimeter对流动沙丘不同干沙层厚度下的土壤水分蒸发作了测定与分析,结果表明:当干沙层厚度发育达到5 cm以上时,流动沙丘干沙层厚度成为土壤水分蒸发的决定因素。随着干沙层厚度的增加,土壤蒸发量逐渐降低;各观测日的蒸发抑制率随着干沙层厚度的增大而增大;5 cm的干沙层对蒸发的抑制作用最大可达70.6%,30 cm的干沙层则最大可达92.38%;干沙层厚度与土壤蒸发量之间存在显著的线性关系。各气象因子以及湿沙层不同深度土壤体积含水率对土壤蒸发量的影响作用很小,相关分析均没有达到显著水平。

关 键 词:蒸发  流动沙丘  干沙层厚度  气象因素
文章编号:1000-6060(2006)04-0523-04
收稿时间:2005-12-12
修稿时间:2006-03-14

Influence of dry sand bed thickness on soil moisture evaporation in mobile dune
LIU Xin-ping,ZHANG Tong-hui,ZHAO Ha-lin,HE Yu-hui,YUN Jian-ying,LI Yu-qiang.Influence of dry sand bed thickness on soil moisture evaporation in mobile dune[J].Arid Land Geography,2006,29(4):523-526.
Authors:LIU Xin-ping  ZHANG Tong-hui  ZHAO Ha-lin  HE Yu-hui  YUN Jian-ying  LI Yu-qiang
Institution:Nairnan Desertification Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000 Gansu , China
Abstract:The soil moisture evaporation under the different thickness dry sand bed in mobile dune is measured and analyzed with Micro-lysimeter.The result shows that: when the dry sand bed thickness is more than 5cm,the dry sand bed thickness becomes dominant factor of soil moisture evaporation in mobile dune.With the dry sand bed thickness increasing,the evaporation quantity decrease gradually;the suppression rate of evaporation increases with the dry sand bed thickness increasing;there exists a significant linear relation between the dry sand bed thickness and evaporation quantity.The influence of meteorological factors and different depth soil moisture on evaporation is very small;the difference is not significant between the meteorological factors and evaporation quantity,also the different depth soil moisture and evaporation quantity.
Keywords:evaporation  mobile dune  dry sand bed thickness  meteorological factor
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