子午岭地区坡面浅沟侵蚀临界模型研究  

Predicting Ephemeral Gully Erosion on Hillslopes of Ziwuling Area

作　　者：丁晓斌[1,2] 郑粉莉[1,2] 王彬[1,2] 张鹏[1,2] 陈吉强[1,2] 

机构地区：[1]西北农林科技大学资源环境学院,陕西杨凌712100 [2]中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌712100

出　　处：《水土保持通报》2011年第3期122-125,201,共5页Bulletin of Soil and Water Conservation

基　　金：国家自然科学基金项目"黄土丘陵区发育活跃期切沟侵蚀过程研究"(40871137);国家基础研究发展计划项目"不同类型区土壤侵蚀过程与机理"(2007CB407201)

摘　　要：利用子午岭地区梁坡高精度的GPS(Trimble 5700)实测数据对国内外已有的浅沟侵蚀临界模型进行了验证。结果表明,已有浅沟侵蚀临界模型模拟的子午岭地区浅沟侵蚀分布面积或大于实际浅沟侵蚀区的10%～40%,或小于实际的20%～35%。基于子午岭地区实测的梁坡GPS数据建立高分辩率的DEM,构建了适用于子午岭地区的浅沟侵蚀临界模型。利用实测GPS数据对所建浅沟侵蚀临界模型进行验证,发现用新建的浅沟侵蚀临界模型模拟的研究区梁坡浅沟侵蚀分布区与野外实际浅沟侵蚀分布区非常吻合,其误差仅为5%。Based on high-precision GPS（Trimble 5700） measurement data on hillslopes of Ziwuling area,this paper validated the existing models for predicting ephemeral gully erosion thresholds.The results show that the existing models were 10%～40% over-predicting or 20%～35% under-predicting of the distribution area of ephemeral gully erosion on hillslopes.A new critical model for predicting ephemeral gully erosion on hillslopes was then established through the high-solution DEM generated by GPS,GIS and statistical analysis.The GPS measurement data on hillslopes of the Ziwuling area were then used to validate the newly established critical model.The results show that the new model well predicted the distribution area of ephemeral gully erosion on hillslopes with a low relative error of 5%.

关 键 词：浅沟侵蚀 临界模型 高精度GPS测量 子午岭地区 

分 类 号：S157[农业科学—土壤学]