CLC number: TU433
On-line Access: 2024-08-27
Received: 2023-10-17
Revision Accepted: 2024-05-08
Crosschecked: 2016-06-28
Cited: 0
Clicked: 4397
Citations: Bibtex RefMan EndNote GB/T7714
Jie Xu, Chao Zhou. A simple model for the hysteretic elastic shear modulus of unsaturated soils[J]. Journal of Zhejiang University Science A, 2016, 17(7): 589-596.
@article{title="A simple model for the hysteretic elastic shear modulus of unsaturated soils",
author="Jie Xu, Chao Zhou",
journal="Journal of Zhejiang University Science A",
volume="17",
number="7",
pages="589-596",
year="2016",
publisher="Zhejiang University Press & Springer",
doi="10.1631/jzus.A1600300"
}
%0 Journal Article
%T A simple model for the hysteretic elastic shear modulus of unsaturated soils
%A Jie Xu
%A Chao Zhou
%J Journal of Zhejiang University SCIENCE A
%V 17
%N 7
%P 589-596
%@ 1673-565X
%D 2016
%I Zhejiang University Press & Springer
%DOI 10.1631/jzus.A1600300
TY - JOUR
T1 - A simple model for the hysteretic elastic shear modulus of unsaturated soils
A1 - Jie Xu
A1 - Chao Zhou
J0 - Journal of Zhejiang University Science A
VL - 17
IS - 7
SP - 589
EP - 596
%@ 1673-565X
Y1 - 2016
PB - Zhejiang University Press & Springer
ER -
DOI - 10.1631/jzus.A1600300
Abstract: Considering the great importance of the elastic shear modulus G0 of unsaturated soils to the serviceability of many geo-structures in geo-energy and geo-environmental engineering, some semi-empirical models have been reported for the G0 of unsaturated soils. Existing models require at least three parameters and the calibration of the model parameters requires extensive time-consuming unsaturated soil tests. In this study, a simple semi-empirical model is proposed for the hysteretic G0 of unsaturated soils, requiring only two parameters. The constitutive variables of the mean Bishop’s stress and a bonding variable are adopted for considering the average stress between soil particles and the additional normal forces between soil particles provided by water menisci. The derived equation is applied to simulate the G0 of unsaturated silts and sands. Comparisons between the measured and calculated results demonstrate that the proposed equation is able to describe the influences of various factors on G0, including mean net stress, suction, wetting-drying, and void ratio.
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