At-rest lateral earth pressure of compacted expansive soils: Experimental investigations and prediction approach

被引:19
作者
Han, Zhong [1 ,2 ,3 ]
Zhang, Pan [3 ]
Zou, Weilie [1 ,2 ]
Fan, Kewei [4 ]
Vanapalli, Sai K. [3 ]
Wan, Lianglong [5 ]
机构
[1] Wuhan Univ, Sch Civil Engn, Wuhan, Peoples R China
[2] Wuhan Univ, Key Lab Rock Mech Hydraul Struct Engn, Minist Educ, Wuhan, Peoples R China
[3] Univ Ottawa, Dept Civil Engn, Ottawa, ON, Canada
[4] Hohai Univ, Key Lab Minist Educ Geomechan & Embankment Engn, Nanjing, Peoples R China
[5] Residence Engn Management Stn Shenzhen Municipal, Shenzhen, Peoples R China
基金
中国国家自然科学基金;
关键词
Lateral earth pressure; Expansive soil; Soaking; Vertical stress; Swelling pressure; SWELLING BEHAVIOR; CLAY; STRESS; COEFFICIENT; BENTONITE;
D O I
10.1016/j.jrmge.2023.10.014
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This paper presents experimental studies on a compacted expansive soil, from Nanyang, China for investigating the at-rest lateral earth pressure sigma(L) of expansive soils. The key studies include (i) relationships between the aL and the vertical stress sigma(V) during soaking and consolidation, (ii) the influences of initial dry density p(d0) and moisture content w(0) on the vertical and lateral swelling pressures at no swelling strain (i.e. sigma(V0) and sigma(L0)), and (iii) evolution of the sigma(L) during five long-term wetting-drying cycles. Experimental results demonstrated that the post-soaking sigma(L)-sigma(V) relationships are piecewise linear and their slopes in the passive state (sigma(L) > sigma(V)) and active state (sigma(L) < sigma(V)) are similar to that of the consolidation sigma(L)-sigma(V) relationships in the normal- and over-consolidated states, respectively. The soaking sigma(L)-sigma(V) relationships converge to the consolidation sigma(L)-sigma(V) relationships at a threshold aV where the interparticle swelling is restrained. The sigma(L0) and sigma(V0) increase monotonically with p(d0); however, they show increasingthen-decreasing trends with the w(0). The extent of compaction-induced swelling anisotropy, which is evaluated by sigma(L0)/sigma(V0), reduces with an increase in the compaction energy and molding water content. The sigma(L) reduces over moisture cycles and the stress relaxation in the sigma(L) during soaking is observed. An approach was developed to predict the at-rest soaking sigma(L)-sigma(V) relationships, which requires conventional consolidation and shear strength properties and one measurement of the sigma(L)-sigma(V) relationships during soaking. The proposed approach was validated using the results of three different expansive soils available in the literature. (c) 2024 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/ licenses/by-nc-nd/4.0/).
引用
收藏
页码:1425 / 1435
页数:11
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