Example: dental hygienist

Numerical Simulation and Centrifuge Modeling of …

Numerical Modeling Computed Deviatoric Strain Pore Water Pressure Buildup Computed Deviatoric Stress Deviatoric Stress Loading Introduction The development of excess pore pressures during an earthquake may lead to soil softening, loss of stability and bearing failures. The ability of the constitutive model to predict permanent volume changes during cyclic loading is a major factor in seismic analysis. This poster presents the application of a kinematic cyclic plasticity model in the Simulation of sand liquefaction and the validation of the Numerical study by Centrifuge -based experimental results.

Numerical Modeling Computed Deviatoric Strain Pore Water Pressure Buildup Computed Deviatoric Stress Deviatoric Stress Loading Introduction The development of excess pore pressures during an earthquake may lead to soil

Information

Domain:

Source:

Link to this page:

Please notify us if you found a problem with this document:

Other abuse

Transcription of Numerical Simulation and Centrifuge Modeling of …

1 Numerical Modeling Computed Deviatoric Strain Pore Water Pressure Buildup Computed Deviatoric Stress Deviatoric Stress Loading Introduction The development of excess pore pressures during an earthquake may lead to soil softening, loss of stability and bearing failures. The ability of the constitutive model to predict permanent volume changes during cyclic loading is a major factor in seismic analysis. This poster presents the application of a kinematic cyclic plasticity model in the Simulation of sand liquefaction and the validation of the Numerical study by Centrifuge -based experimental results.

2 Numerical Simulation and Centrifuge Modeling of Sand Liquefaction Yu (Amanda) Bao, , , and Andrew Rietz Rochester Institute of Technology (se c)Excess pore Water Pressure Ratio (u/p) Centrifuge TestComputedk Numerical Simulation Results Experimental Modeling 40-th Scale Centrifuge Model LVDTPore water pressure transducerAccelerometerLooseliquefiable water pressure transducerAccelerometerLooseliquefiable Table Input Motion (sec)Input Acceleration (g)Pore Water Pressure -1001020304050607080901000246810 Tim e (sec)Excess Pore Water Pressure (Kpa) Results Conclusions Modeling experiments and Numerical Simulation of a liquefiable sand layer are conducted and compared.

3 Both the Numerical and experimental results show that the development of pore water pressure and liquefaction are a consequence of the base excitation. computed results showed good agreement with the experimental data. developed fuzzy-set plasticity formulation and computational procedure are an effective means to assess liquefaction potential and liquefaction-related deformations. References: , Y. and Sture, S., Numerical Modeling of cyclic mobility based on fuzzy-set concepts in plasticity theory , Computers and Geotechnics, Vol. 38, Issue 3, 375-382, 2011. , Y.

4 And Sture, S., Application of a kinematic-cyclic plasticity model in simulating sand liquefaction , International Journal of Advances in Engineering Sciences and Applied Mathematics, Vol. 2, Issue 3, 119-124, 2010. , L., Bao, Y., Ni, C. K. and Ko, H. Y., Seismic Centrifuge modelling of earth dams , Geomechanics and Geoengineering, , Issue 4, 247-257, 2010. Modeling experiments and Numerical Simulation of a liquefiable sand layer are conducted and compared. Both the Numerical and experimental results show that the development of pore water pressure and liquefaction are a consequence of the base excitation.

5 Computed results showed good agreement with the experimental data. developed fuzzy-set plasticity formulation and computational procedure are an effective means to assess liquefaction potential and liquefaction-related deformations. Building Collapse Land Spreading -25-20-15-10-5051015202502468101214 Time (sec)Deviatoric Stress q (Kpa)Test StrainDeviatoric StrainVolumetric Strain-25-20-15-10-505101520250246810121 4 Deviatoric Stress q (Kpa) Time (sec) Test InputComputedk Fuzzy-Set Plasticity Model Deviatoric Membership Function Volumetric Membership Function


Related search queries