Technical Papers
Jun 24, 2022

DEM-Based Study on the Mechanical Behaviors of Pore-Filling MHBS under Drained True Triaxial Conditions Varying the Intermediate Stress Ratio of Constant Mean Effective Stresses

Publication: International Journal of Geomechanics
Volume 22, Issue 9

Abstract

Methane hydrate-bearing soils (MHBS) are natural soil deposits that contain methane hydrate (MH) in the pores and have attracted a huge amount of attention as alternative energy to study mechanical properties for realizing large-scale commercial extraction. Especially, MHBS respond to applied loads under complex stress conditions, that is, the effect of the intermediate stress ratio on mechanical characteristics of MHBS. The effect of different values of intermediate stress ratios on the geomechanical responses of pore-filling MHBS was analyzed using the distinct element method (DEM). MH clusters are cemented together as agglomerates of spheres, which fill into the voids of the soil specimen according to the MH saturation. Then, the numerical pore-filling MHBS experimented with different loading paths of the true triaxial tests. Finally, the effects of the intermediate stress ratio on the mechanical characteristics of pore-filling MHBS were analyzed from two aspects, that is, macromechanical responses and micromechanical responses. The results showed that there were correlation analyses between the variations in the strong fabric and principal stresses. The friction angle increased with the intermediate stress ratio until it reached a peak value, and decreased thereafter. The Lade–Duncan criterion is approximately suitable to describe the three-dimensional strength of MHBS.

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Data Availability Statement

Data shown in Figs. 5–8 that support the findings of this study are available from the corresponding author upon reasonable request.

Acknowledgments

The research was funded by the fellowship of the China Postdoctoral Science Foundation (Grant Nos. 2019M651580 and 2020T130471), the Natural Science Foundation Committee Program of China (Grant No. 41907245). Thanks for all the support.

Notation

The following symbols are used in this paper:
b
intermediate principal stress ratio;
C
number of contacts;
c
cohesion;
D
mean diameter of the soil particle;
d
dilatancy index;
dɛd
increment on the equivalent deviatoric strain;
dɛv
change in volumetric strain;
Ec
Young’s modulus of the soil;
ea
void ratio in the agglomerate;
ecr
void ratio in the critical state;
F11s
major principal fabric;
F22s
intermediate principal fabric;
F33s
minor principal fabric;
Iuf
an index to quantify the unbalanced force;
I1
first stress invariants;
I2
second stress invariants;
I3
third stress invariants;
J2
second invariant of the stress tensor;
kf
soil characteristic parameter;
kn
normal contact stiffness;
knsoilp
soil normal contact stiffness;
kssoilp
soil tangential contact stiffness;
k¯n
normal parallel bond stiffness;
k¯s
shear parallel bond stiffness;
knmhp
MH normal contact stiffness;
ksmhp
MH tangential contact stiffness;
k
laboratory constant;
Mcr
critical stress ratio for different b;
Nbr
number of surviving MH bonds in any given state;
Nc
number of contacts;
Ncs
number of the strong contacts;
Ncr
number of MH bonds in the initial state;
Np
number of particles;
N
number of MH agglomerates required in the pore-filling MHBS;
N1
number of particles with only one contact;
N0
number of particles with no contacts;
nis
component of the unit vector ns at the contact between grains i and j;
np
number of methane hydrate particles in the MHC;
P
mean effective stress;
pa
atmospheric pressure;
q
generalized shear stress;
Ra
equivalent radius of the sphere of equal volume;
r
radius of a methane hydrate particle;
Smh
MH saturation;
Va
volume of a single MH cluster;
Vmh
MH volume;
Vv
total pore volume;
V
changes in the volume of the MHBS;
Zm
mechanical coordination number;
Z
average coordination number;
μsoilp
Soil interparticle coefficient of friction;
μmhp
MH interparticle coefficient of friction;
η
stress ratio;
σ¯c
normal parallel bond strengths;
σ1
major principal stress;
σ2
intermediate principal stress;
σ3
minor principal stresses;
ɛ1
major principal strain;
ɛ2
intermediate principal strain;
ɛ3
minor principal strain;
ɛd
equivalent deviatoric strain;
ɛv
volumetric strain;
V
initial volume of the MHBS;
λ
slope of the CSL;
λ¯
ratio of the parallel bond radius to the ball radius;
ξ
material constant;
Γ
intercept of the CSL;
θ
Lode angles of the soil;
σπ
π plane compressive stress;
τπ
π plane shear stress;
τ¯c
shear parallel bond strengths; and
φ
internal friction angle.

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International Journal of Geomechanics
Volume 22Issue 9September 2022

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Received: Apr 17, 2021
Accepted: Feb 12, 2022
Published online: Jun 24, 2022
Published in print: Sep 1, 2022
Discussion open until: Nov 24, 2022

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College of Civil Engineering, Tongji Univ., Shanghai 200092, China; State Key Laboratory for Disaster Reduction in Civil Engineering, Tongji Univ., Shanghai 200092, China; Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji Univ., Shanghai 200092, China. Email: [email protected]
Professor, College of Civil Engineering, Tongji Univ., Shanghai 200092, China; State Key Laboratory for Disaster Reduction in Civil Engineering, Tongji Univ., Shanghai 200092, China; Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji Univ., Shanghai 200092, China; Dept. of Geotechnical Engineering, Tongji Univ., Shanghai 200092, China. Email: [email protected]
Mingliang Zhou [email protected]
College of Civil Engineering, Tongji Univ., Shanghai 200092, China; State Key Laboratory for Disaster Reduction in Civil Engineering, Tongji Univ., Shanghai 200092, China; Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji Univ., Shanghai 200092, China (corresponding author). Email: [email protected]

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