Effect of clay content to the strength of gravel soil in the source region of debris flow

doi:10.1007/s11629-018-4911-8

CORC > 成都山地灾害与环境研究所 > 中国科学院水利部成都山地灾害与环境研究所 > Journal of Mountain Science > Journal of Mountain Science-2018 > Vol15 No.10

	Effect of clay content to the strength of gravel soil in the source region of debris flow
	Chen Ning-sheng; Gao Yan-chao; Yang Cheng-lin; Hu Gui-sheng
刊名	JOURNAL OF MOUNTAIN SCIENCE
	2018
卷号	15 期号:10 页码:2320-2334
关键词	Debris flows Gravel soil Clay content Maximum shear stress Pore water pressure
ISSN号	1672-6316
DOI	10.1007/s11629-018-4911-8
文献子类	Article
英文摘要	The production of runoff in the source area of a debris flow is the consequence of a reduction in soil strength. Gravel soil is widely distributed in the source region, and the influence of its clay content on soil strength is one of the important questions regarding the formation mechanism of debris flows. In this paper, the clay content in gravel soil is divided into groups of low clay content (1%, 2, 5%), moderate clay content (3.75%, 5.00%, 6.25%, 7.5%) and high clay content (10.0%, 12.5%, 15%). Tests of the unconsolidated undrained shear strength and consolidated drained shear strength were performed. The unconsolidated undrained shearing (UU) experiment simulates the rapid shear failure of loose gravel soil under the conditions of brief heavy rainfall. The consolidated drained shearing (CD) experiment simulates creep failure of consolidated sediment during extended rainfall. The pore water pressure first increased and then decreased as the clay content increased, and the increase in pore pressure was relatively high in the gravel soil sample when the clay content is in the range of 3.25-7.50%, and stress in the gravel soil is relatively low for a moderate clay content. Gravelly soils with a moderate clay content are more prone to debris-flow initiation. This paper presents a mathematical formula for the maximum shear stress and clay content of gravel soil under two conditions. The key processes whereby the soil fails and triggers a debris flow-volume contraction of soil, expansion of clay soil, and rise of pore pressure-cause reductions in the soil friction force and enhancement of the water content in the clay particles, and subsurface erosion of soil reduces the soil viscosity, which eventually reduces the soil strength so that the soil loses its stability, liquefies and generates a debris flow.
电子版国际标准刊号	1993-0321
语种	英语
WOS记录号	WOS:000447295900018
内容类型	期刊论文
源URL	[http://ir.imde.ac.cn/handle/131551/46335]
专题	Journal of Mountain Science_Journal of Mountain Science-2018_Vol15 No.10
推荐引用方式 GB/T 7714	Chen Ning-sheng,Gao Yan-chao,Yang Cheng-lin,et al. Effect of clay content to the strength of gravel soil in the source region of debris flow[J]. JOURNAL OF MOUNTAIN SCIENCE,2018,15(10):2320-2334.
APA	Chen Ning-sheng,Gao Yan-chao,Yang Cheng-lin,&Hu Gui-sheng.(2018).Effect of clay content to the strength of gravel soil in the source region of debris flow.JOURNAL OF MOUNTAIN SCIENCE,15(10),2320-2334.
MLA	Chen Ning-sheng,et al."Effect of clay content to the strength of gravel soil in the source region of debris flow".JOURNAL OF MOUNTAIN SCIENCE 15.10(2018):2320-2334.