An evaluation method for internal erosion potential of gravelly soil based on particle size distribution

被引:0
作者
Qin Zhu
Li-jun Su
Zhen-yu Liu
Bin Wang
机构
[1] Chinese Academy of Sciences,Key Laboratory of Mountain Hazards and Earth Surface Process, Institute of Mountain Hazards and Environment
[2] University of Chinese Academy of Sciences,undefined
[3] China-Pakistan Joint Research Centre on Earth Sciences,undefined
来源
Journal of Mountain Science | 2022年 / 19卷
关键词
Internal erosion; Gravelly soil; Evaluation method; Particle size distribution; Coarse particle content;
D O I
暂无
中图分类号
学科分类号
摘要
Internal erosion occurs when fine particles escape from the soil driven by seepage flow, which is considered to be the crucial factor causing the failure of earth structures filled with gravelly soil. The objective of this paper is to suggest an appropriate method to assess internal erosion potential of gravelly soil. By analyzing the sensitivity of soil material to internal erosion, the variable (Dc15/df85)max and the content of coarse particles (Pc) are selected as the evaluation indexes (Dc15 and df85 are the diameters of 15% mass passing in the coarse component and 85% mass passing in the fine component, respectively). A series of gravelly soils with different particle size distributions are tested for internal erosion by the self-made permeameter. Based on the test results, an evaluation method for the internal erosion of gravelly soil is proposed. Gravelly soil is prone to internal erosion when 60% ≤ Pc < 95% and (Dc15/df85)max > 9.5. The proposed method shows good accuracy in evaluating the internal erosion of 36 soil samples from other studies, which confirms the reliability of the method. The proposed method makes it possible to accurately assess internal erosion of gravelly soil, and an alternative method is provided for engineers to determine whether there is a risk of internal erosion in earth structures consisting of gravelly soil.
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页码:1203 / 1214
页数:11
相关论文
共 121 条
[1]  
Ahmadi M(2020)DEM modelling to assess internal stability of gap-graded assemblies of spherical particles under various relative densities, fine contents and gap ratios Comput Geotech 126 103710-67
[2]  
Shire T(2008)Experimental parametric study of suffusion and backward erosion J Geotech Geoenviron 134 57-97
[3]  
Mehdizadeh A(2003)Determining grain size distribution of the material composing landslide dams in the northern apennines: sampling and processing methods Eng Geol 69 83-583
[4]  
Bendahmane F(2013)Extended internal stability criteria for soils under seepage Soils Found 53 569-1467
[5]  
Marot D(2013)Critical hydraulic gradients of internal erosion under complex stress states J Geotech Geoenviron 139 1454-85
[6]  
Alexis A(2014)Liquefaction characteristics of gap-graded gravelly soils in k Soil Dyn Earthq Eng 56 74-176
[7]  
Casagli N(1996) condition Can Geotech J 33 168-194
[8]  
Ermini L(2009)Migration of fines in 0–20 mm crushed base during placement, compaction, and seepage under laboratory conditions Int J Geomech 9 187-431
[9]  
Rosati G(2017)Seepage-induced erosion in granular soil and consequent settlements J Mt Sci 14 417-10
[10]  
Chang DS(2017)Experimental study on the moving characteristics of fine grains in wide grading unconsolidated soil under heavy rainfall Eng Geol 230 1-160