Technical Papers
Nov 9, 2021

Predicting Resilient Modulus of Unsaturated Subgrade Soils Considering Effects of Water Content, Temperature, and Hydraulic Hysteresis

Publication: International Journal of Geomechanics
Volume 22, Issue 1

Abstract

The resilient modulus, MR, of subgrade soils is an important parameter in design and analysis of pavements. Subgrade soils are often unsaturated and can experience a wide range of suctions due to changes in water content and temperature induced by seasonal variation and climatic events. Laboratory- and field-measured data show that MR is affected by stress level, water content, temperature, and hydraulic hysteresis. However, none of the existing models explicitly accounts for the effect of temperature nor can they accurately predict MR in high suctions. In this study, a generalized model is developed that can predict MR while incorporating water content, temperature, changes in deviatoric stress, and hydraulic hysteresis. A base model is first presented to predict the variation of MR in regard to water content and is dictated by two distinct water retention mechanisms—capillarity and adsorption. Accordingly, a two-part model is employed to separately account for changes in MR with water content under capillary and adsorption mechanisms. This feature allows the proposed model to accurately capture the characteristics of MR over the entire range of suction. The base model is then extended to incorporate the effects of temperature, changes in deviatoric stress, and hydraulic hysteresis. The proposed model exhibited an excellent performance upon validation against a total of 218 experimentally measured MR values reported in the literature spanning 14 different test sets on nine different soils tested under different conditions. The predictive errors are significantly lower than that from four alternative models, including the model in the Mechanistic-Empirical Pavement Design Guide (MEPDG). The presented model is straightforward and can be used in practice to predict the MR of subgrade soils considering concurrent changes in water content and temperature.

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Acknowledgments

This material is based upon work supported in part by the National Science Foundation under Grant No. CMMI-1951636. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation.

Notation

The following symbols are used in this paper:
aFX, nFX, mFX
Fredlund and Xing (1994) SWRC model’s fitting parameters;
kh
fitting parameter considering the effect of hydraulic hysteresis [Eq. (23)];
km
fitting parameter considering the changes in moisture content [Eq. (2)];
k1, k2, k3
MEPDG model fitting parameters [Eq. (1)];
l1, l2
Yang et al. (2005) model fitting parameters [Eq. (3)];
m
SWRC fitting parameters reflecting adsorption strength;
mM
fitting parameter considering the effect of capillary water content [Eq. (11)];
MMc
maximum resilient modulus due to capillary mechanism;
MMd
maximum resilient modulus at dry state;
MR
resilient modulus;
(MR)D
resilient modulus along the main drying path;
(MR)W
resilient modulus along the main wetting path;
MR,OPT
resilience modulus at optimum moisture content;
MR,SAT
resilient modulus at saturated condition;
Mw
molar volume of water;
m1, m2, m3
Liang et al. (2008) model fitting parameters [Eq. (4)];
n
SWRC fitting parameters related to soil particle size and distribution;
n1, n2, n3, n4
Cary and Zapata (2011) model fitting parameters [Eq. (5)];
Pa
atmospheric pressure;
R
universal gas constant;
R2
coefficient of determination;
RH
relative humidity;
RMSE
root mean square error;
S
degree of saturation;
SOPT
degree of saturation at optimum moisture content;
T
temperature;
ΔhT
enthalpy of immersion per unit area;
ΔhTr
enthalpy of immersion per unit area at the reference temperature;
Δuw‐sat
buildup of pore-water pressure under saturated condition;
α
SWRC fitting parameters related to soil air entry value;
α
soil-water contact angle;
β, βTr
regression parameters of Eq. (18);
ɛr
recoverable strain;
κ
fitting parameter considering the effect of changes in deviatoric stress [Eq. (15)];
θ
volumetric water content;
θa,max
maximum adsorption water content;
θb
bulk stress;
θnet
net bulk stress;
θs
saturated volumetric water content;
ξ
Han and Vanapalli (2015) model fitting parameter [Eq. (6)];
σd
deviatoric stress;
τoct
octahedral shear stress;
χ
Bishop’s effective stress parameter;
ψ
suction;
ψc
mean cavitation pressure;
ψD
suction along main wetting path;
ψmax
maximum suction;
ψOPT
suction at optimum moisture content;
ψTr
reference temperature; and
ψW
suction along main drying path.

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International Journal of Geomechanics
Volume 22Issue 1January 2022

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Received: Jul 28, 2020
Accepted: Sep 11, 2021
Published online: Nov 9, 2021
Published in print: Jan 1, 2022
Discussion open until: Apr 9, 2022

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Ph.D. Student, Richard A. Rula School of Civil and Environmental Engineering, Mississippi State Univ., Mississippi State, MS 39762. ORCID: https://orcid.org/0000-0002-5273-2073. Email: [email protected]
CEE Advisory Board Endowed Professor and Professor, Richard A. Rula of Civil and Environmental Engineering, Mississippi State Univ., Mississippi State, MS 39762 (corresponding author). ORCID: https://orcid.org/0000-0001-8883-4533. Email: [email protected]

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