TY - JOUR
T1 - Coupled hydro-mechanical analysis of expansive soils
T2 - Parametric identification and calibration
AU - Rawat, Abhishek
AU - Lang, Linzhi
AU - Baille, Wiebke
AU - Dieudonné, Anne-Catherine
AU - Collin, Frederique
PY - 2020
Y1 - 2020
N2 - A methodology for identifying and calibrating the material parameters for a coupled hydro-mechanical problem is presented in this paper. For validation purpose, a laboratory-based water infiltration test was numerically simulated using finite element method (FEM). The test was conducted using a self-designed column-type experimental device, which mimicked the wetting process of a candidate backfill material in a nuclear waste repository. The real-time measurements of key state variables (e.g. water content, relative humidity, temperature, and total stresses) were performed with the monitoring sensors along the height of cylindrical soil sample. For numerical simulation, the modified Barcelona Basic Model (BBM) along with soil-water retention model for compacted bentonite was used. It shows that the identified model parameters successfully captured the moisture migration process under an applied hydraulic gradient in a bentonite-based compacted soil sample. A comparison between the measured and predicted values of total stresses both in axial and lateral directions along with other state variables revealed that heterogeneous moisture content was distributed along the hydration-path, resulting in non-uniform stress-deformation characteristics of soil.
AB - A methodology for identifying and calibrating the material parameters for a coupled hydro-mechanical problem is presented in this paper. For validation purpose, a laboratory-based water infiltration test was numerically simulated using finite element method (FEM). The test was conducted using a self-designed column-type experimental device, which mimicked the wetting process of a candidate backfill material in a nuclear waste repository. The real-time measurements of key state variables (e.g. water content, relative humidity, temperature, and total stresses) were performed with the monitoring sensors along the height of cylindrical soil sample. For numerical simulation, the modified Barcelona Basic Model (BBM) along with soil-water retention model for compacted bentonite was used. It shows that the identified model parameters successfully captured the moisture migration process under an applied hydraulic gradient in a bentonite-based compacted soil sample. A comparison between the measured and predicted values of total stresses both in axial and lateral directions along with other state variables revealed that heterogeneous moisture content was distributed along the hydration-path, resulting in non-uniform stress-deformation characteristics of soil.
KW - Backfill material
KW - Compacted bentonite
KW - Constitutive modeling
KW - Deep geological repository
KW - Hydro-mechanical coupling
KW - Water infiltration test
UR - http://www.scopus.com/inward/record.url?scp=85085195025&partnerID=8YFLogxK
U2 - 10.1016/j.jrmge.2019.12.013
DO - 10.1016/j.jrmge.2019.12.013
M3 - Article
AN - SCOPUS:85085195025
SN - 1674-7755
VL - 12
SP - 620
EP - 629
JO - Journal of Rock Mechanics and Geotechnical Engineering
JF - Journal of Rock Mechanics and Geotechnical Engineering
IS - 3
ER -