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[1]YANG Tao,WANG De-xiang,LIU Ya-juan,et al.The Dynamical Changes of Soil Water Holding Capacity of Different Vegetation Types in Loess Hilly Region[J].Research of Soil and Water Conservation,2008,15(06):81-84.

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The Dynamical Changes of Soil Water Holding Capacity of Different Vegetation Types in Loess Hilly Region

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 15 Number of periods: 2008 06 Page number: 81-84 Column: Public date: 2008-12-20

Title:: The Dynamical Changes of Soil Water Holding Capacity of Different Vegetation Types in Loess Hilly Region

Author(s):: YANG Tao^1,2, WANG De-xiang³, LIU Ya-juan⁴, WEI Guo-liang⁵; 1. College of Natural Resources and Environment, Northwest A & F University, Yangling, Shaanxi 712100, China;
2. Institute for Control Sand of Shaanxi Province, Yulin, Shaanxi 719000, China;
3. College of Forestry, Northwest A & F University, Yangling, Shaanxi 712100, China;
4. Yulin City Work Station of Foresty, Yulin, Shaanxi 719000, China;
5. Qinghai University, Xi’ning 810003, China

Keywords:: Loess hilly region; vegetation types; soil water content; dynamical change

CLC:: S152.7

DOI:: -

Abstract:: Water is the primary limiting factor of vegetation and plant growth in the semi-arid Loess Plateau region.Vegetation is one of the factors which affecting soil water content.From 1982 to 1991,based on the observation of soil water content of different vegetation type in Shangbian valley,the changes of vertical soil water content,seasonal and inter-annual change of different vegetation types are analyzed in Loess Hilly area,as well as the relationships of annual rainfall and soil water content.The vegetation type vertical changes of water content in 0-100cm changes were: 0-30cm soil layer,farmland>woodland>farming>pasture>shrub land,30-50cm soil layer,farmland>pasture>shrub land>woodland>farming; 50-100cm soil layer,pasture>shrub land>farmland>woodland>wasteland.

References:: [1] 吴钦孝,杨文治.黄土高原植被建设与持续发展[M].北京: 科学出版社,1998.
[2] 徐化成,易宗文.华北低山区土壤水分季节变化与林分生长关系[J].林业科学,1979,15(2):97-104.
[3] 杨文治.黄土高原土壤水分状况分区与造林问题[J].水土保持通报,1981,1(2):13-19.
[4] 李凯荣.刺槐人工林地土壤水分下渗研究[J].西北林学院学报,1998,13(2):26-29.
[5] 单长卷,梁宗锁,郝文芳.黄土高原刺槐林生长于土壤水分分析研究进展[J].西北植物学报,2003,23(8):1341-1346.
[6] 李艳梅,王克勤.人工植被土壤水分状况与动态研究进展[J].西南林学院学报,2003,23(3):68-71.
[7] 李洪建,王孟本,柴宝峰.黄土高原土壤水分变化的时空特征分析[J].应用生态学报,2003,14(4): 515-519.
[8] 赵名茶.黄土高原降水的季节性指标及其与作物水分亏缺的关系[J].自然资源学报,1990,5(3):218-228.
[9] 原焕英,许喜明.黄土高原半干旱丘陵沟壑区人工林土壤水分动态研究[J].西北林学院学报,2004,19(2):5-8.
[10] 杨新民,杨文治.黄土丘陵区人工林地土壤水分平衡初探[J].林业科学,1989,25(6):549-553.
[11] Coronator F R,Rtiler M B.Precipitation and landscape related effects on soil moisture in semi-arid range lands Patagonia[J].Journal of Arid Environment,1996,34:1-3.
[12] 李遇春,冯佐乾.固原市原州区叠叠沟小流域五种植被类型下土壤水分动态研究[J].现代农业科技,2006(12):8-12.

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