Erodibility of soil at the gully head in Yuanmou dry-hot valley, China
Nan, Ling1,3; Chena, An-Qiang1,3; Liu, Gang-Cai1,2
2011
会议日期2010-12
会议地点Qingdao
关键词gully erodibility slaking shearstrength
卷号7752
DOI10.1117/12.887704
页码77520Y
国家China
英文摘要In the recent years, gully erosion attracted increasing attention from scientists. However, there were few studies on the soil erodibility/anti- erodibilty for the gully erosion. Based on the principle ofgeotechnical slaking test, a new set of test apparatus had been designed and applied on the study oferodibility of soil at the gully head. In this experiment, 6 typical gully heads had been chosen. Soil at thedifferent depth of each gully head had been sampled by the foil sampler and tested the slaking rate ofthem. Moreover, shear strength of soil at different depth of each gully head had been tested in situ. Theresults showed that gullies developed on the stratified soil or homogeneous soil have different morphological characteristics. At the sharp gully head, the erodibility of underlying soil was lower thanthe overlying soil's. Contrarily, at gradual gully head, the erodibility of underlying soil was not lower thanthe overlying soil's. Moreover, slaking rate of most gullies' soil in the study area is an inverse proportion tothe shear stress. Thus, slaking rate and in-situ shear stress, any of them can be the indicator of theerodibility of soil in the study region. But shear stress is easier to measure in situ. 
源文献作者SPIE
产权排序1
会议录Proceedings of SPIE - The International Society for Optical Engineering
语种英语
ISSN号0277786X
ISBN号9780819482457
内容类型会议论文
源URL[http://ir.imde.ac.cn/handle/131551/25940]  
专题成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
作者单位1.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, China;
2.Key Laboratory of Mountain Hazards and Earth Surface Process, Chinese Academy of Sciences, Chengdu, China;
3.Graduate University of Chinese Academy of Sciences, Beijing, China
推荐引用方式
GB/T 7714
Nan, Ling,Chena, An-Qiang,Liu, Gang-Cai. Erodibility of soil at the gully head in Yuanmou dry-hot valley, China[C]. 见:. Qingdao. 2010-12.
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