节点文献

土壤水分变异对降雨和植被的响应

Responses of soil moisture variations to rainfall and vegetation

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 杨启红陈丽华张富张超波

【Author】 YANG Qi-hong1;CHEN Li-hua1;ZHANG Fu2;ZHANG Chao-bo1.1 Key Laboratory for Soil and Water Conservation & Desertification Combating of Ministry of Education,College of Soil and Water Conservation,Beijing Forestry University,100083,P.R.China;2 Soil and Water Conservation Station of Dingxi City,Gansu Province,743000,P.R.China.

【机构】 北京林业大学水土保持学院水土保持与荒漠化防治教育部重点实验室甘肃省定西市水土保持工作总站

【摘要】 在我国半干旱地区水土流失严重的黄土高原,开展土壤水分的时空变异研究有着极其重要的生态意义,是土地可持续利用的基础。该文利用时间序列分析方法,研究了黄土高原丘壑区降雨、植被对土壤水分特征变化的影响。结果表明,红豆草和豌豆的表层土壤含水量对降雨响应速度快于油松土壤含水量;水分入渗增湿与同期降雨量密切相关;土壤含水量对降雨的响应时间随土层深度的增加而变长。

【Abstract】 Soil moisture is a basic survival factor for plants.Soil erosion is serious in the Loess Plateau of China.The research on the temporal and spatial variation of soil moisture has an important ecological significance and it is also the basis of sustainable land use.The method of time-series analysis was used to study the effects of rainfall and vegetation on soil moisture characteristics in the hilly areas on the Loess Plateau.The results indicated that the response rates of soil moisture content for Onobrychis viciaefolia and Pisum sativum in surface layer were more quickly than that for Pinus tabulaeformis.The infiltrating moisture was closely related to the rainfall amount.The response time of soil moisture content increased with the increase of soil depth.

【关键词】 土壤水分降雨植被时间序列
【Key words】 soil moisturerainfallvegetationtime series
【基金】 “十一五”国家科技支撑计划项目(2006BAD03A02、2006BAD09B02--03)
  • 【文献出处】 北京林业大学学报 ,Journal of Beijing Forestry University , 编辑部邮箱 ,2008年S2期
  • 【分类号】S152.7
  • 【被引频次】12
  • 【下载频次】407
节点文献中: 

本文链接的文献网络图示:

本文的引文网络