Pore water pressure increase in loose saturated sand at level sites during three-directional earthquake loading.

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Stresses, strains and pore pressure buildup caused by the ground accelerations are predicted, with due consideration to the nonlinear, anisotropic, elastic-plastic stress path dependent and modulus degrading characteristics exhibited by the soil during undrained cyclic loading.

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December 1983
School of Engineering

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Rensselaer Polytechnic Institute, Troy, NY

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