TY - JOUR
T1 - Behavior of EPS geofoam in true triaxial compression tests
AU - Leo, Chin Jian
AU - Kumruzzaman, M.
AU - Wong, Henry
AU - Yin, Jin H.
PY - 2008
Y1 - 2008
N2 - This paper investigates the behavior of EPS geofoam in a true triaxial apparatus using 70 mmÃÂ70 mmÃÂ140 mm prismatic brick-shaped specimens. The specimens are subjected to different stress paths in the deviator (π) plane by means of stress-controlled loading, in which the axial stress is imposed at a rate of 75 kPa/min in the major principal direction. Stress-strain characteristics and volume change behavior have been recorded, and the yield surface has been deduced from the experimental data. The following observations have also been made for the geofoam: (a) it is an elastoplastic hardening material with plastic contractive volume change under compressive loading, (b) it softens stiffness-wise under confining stress, (c) the onset of contractive volume change corresponds quite well to the proportional limit, and (d) yielding is a slightly decreasing function of the intermediate principal stress. The study found that yielding can be represented reasonably well by a Drucker-Prager yield surface.
AB - This paper investigates the behavior of EPS geofoam in a true triaxial apparatus using 70 mmÃÂ70 mmÃÂ140 mm prismatic brick-shaped specimens. The specimens are subjected to different stress paths in the deviator (π) plane by means of stress-controlled loading, in which the axial stress is imposed at a rate of 75 kPa/min in the major principal direction. Stress-strain characteristics and volume change behavior have been recorded, and the yield surface has been deduced from the experimental data. The following observations have also been made for the geofoam: (a) it is an elastoplastic hardening material with plastic contractive volume change under compressive loading, (b) it softens stiffness-wise under confining stress, (c) the onset of contractive volume change corresponds quite well to the proportional limit, and (d) yielding is a slightly decreasing function of the intermediate principal stress. The study found that yielding can be represented reasonably well by a Drucker-Prager yield surface.
UR - http://handle.uws.edu.au:8081/1959.7/555853
U2 - 10.1016/j.geotexmem.2007.10.005
DO - 10.1016/j.geotexmem.2007.10.005
M3 - Article
SN - 0266-1144
VL - 26
SP - 175
EP - 180
JO - Geotextiles and Geomembranes
JF - Geotextiles and Geomembranes
IS - 2
ER -