TY - GEN
T1 - A Swinging Plane Model for soil liquefaction analysis
AU - Park, S. S.
AU - Byrne, P. M.
AU - Wijewickreme, D.
PY - 2005
Y1 - 2005
N2 - A simplified constitutive model called a Swinging Plane Model is presented for monotonie and cyclic soil response including liquefaction. This model is based on two mobilized planes: a plane of maximum shear stress, which swings, and a horizontal plane which is spatially fixed. By controlling two mobilized planes, the model can simulate the principal stress rotation effect associated with simple shear from different K 0 states, which can significantly influence soil behaviour. The proposed model gives a similar skeleton behaviour for soils having the same mean stress, regardless of K 0, conditions as observed in laboratory tests. The soil skeleton behaviour observed in cyclic drained simple shear tests, including compaction during unloading and dilation at large strain is captured in the model. Undrained monotonic and cyclic response is predicted by imposing the volumetric constraint of the water on the drained or skeleton behaviour. This constitutive model is incorporated into the dynamic coupled stress-flow finite difference program FLAC (Fast Lagrangian Analysis of Continua). The model was first calibrated with drained monotonie and cyclic simple shear tests on Fraser River sand, and verified by comparing predicted and measured undrained monotonie and cyclic behaviour of Fraser River sand.
AB - A simplified constitutive model called a Swinging Plane Model is presented for monotonie and cyclic soil response including liquefaction. This model is based on two mobilized planes: a plane of maximum shear stress, which swings, and a horizontal plane which is spatially fixed. By controlling two mobilized planes, the model can simulate the principal stress rotation effect associated with simple shear from different K 0 states, which can significantly influence soil behaviour. The proposed model gives a similar skeleton behaviour for soils having the same mean stress, regardless of K 0, conditions as observed in laboratory tests. The soil skeleton behaviour observed in cyclic drained simple shear tests, including compaction during unloading and dilation at large strain is captured in the model. Undrained monotonic and cyclic response is predicted by imposing the volumetric constraint of the water on the drained or skeleton behaviour. This constitutive model is incorporated into the dynamic coupled stress-flow finite difference program FLAC (Fast Lagrangian Analysis of Continua). The model was first calibrated with drained monotonie and cyclic simple shear tests on Fraser River sand, and verified by comparing predicted and measured undrained monotonie and cyclic behaviour of Fraser River sand.
UR - http://www.scopus.com/inward/record.url?scp=84868521889&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:84868521889
SN - 9059660285
SN - 9789059660281
T3 - Proceedings of the 16th International Conference on Soil Mechanics and Geotechnical Engineering: Geotechnology in Harmony with the Global Environment
SP - 845
EP - 850
BT - Proceedings of the 16th International Conference on Soil Mechanics and Geotechnical Engineering
T2 - 16th International Conference on Soil Mechanics and Geotechnical Engineering: Geotechnology in Harmony with the Global Environment, ICSMGE 2005
Y2 - 12 September 2005 through 16 September 2005
ER -