利用^(137)Cs技术研究土壤可蚀性的时空变异(英文)  

DETERMINING THE VARIABILITY\=OF SOIL ERODIBILITY FOR\=EROSION PREDICTION

作　　者：李勇[1,2] Frielinghaus M. Bork H.R. 

机构地区：[1]中国科学院山地灾害与环境研究所 [2]中国农业科学院原子能利用研究所 [3]德国农业景观与土地利用研究中心

出　　处：《核农学报》1999年第3期129-136,共8页Journal of Nuclear Agricultural Sciences

摘　　要：土壤可蚀性的研究变异性是当代土壤侵蚀预测预报研究的核心。本文综述了土壤可蚀性变异性研究的进展及存在的问题，提出了利用１３７Ｃｓ法定量测定土壤可蚀性时空变异的新技术。Soil erodibility refers to the susceptibility or resistance of a soil to detachment and transport by erosion for a particular site. Accurate prediction of soil erosion strongly requires a sufficient understanding of the variability in soil erodibility parameters. This paper reviews the existing knowledge on these topics and defines research gaps. In the framework of soil erosion prediction studies it is important to consider soil erodibility at various temporal and spatial scales. Little research has hitherto been conducted on quantitative assessment of spatial variability in soil erodibility and its relation to soil condition factors at different landscape level. But such information on this aspect is crucial for quantitatively describing the paths of erosion and to develop solutions or conceptions to interrupt these paths within the landscape. From this review, it can be concluded that special attention must be paid to the quantitative assessment of soil erodibility at various scales up to the catchment scale. The results of such studies should be used to relate erodibility parameters to soil condition factors that can be measured easily and confidently. Caesium\|137 approach would be a reliable method for determining spatial variability in soil erodibility within the landscape, which has fast, inexpensive and accurate advantages over many classical measuring techniques.

关 键 词：土壤 可蚀性 土壤侵蚀 时空变异 铯137 

分 类 号：S157[农业科学—土壤学]