Location

San Diego, California

Presentation Date

30 Mar 2001, 10:30 am - 12:30 pm

Abstract

The Kobe Earthquake in Japan caused shallow sliding on the upstream slope below the water level of the Kitayama Dam. This paper briefly stated the results of post-earthquake surveys and tests of this earth dam. The FE model of the dam was prepared based on the detailed results of in-situ tests and laboratory material tests. The numerical analysis was performed by the effective stress analysis to simulate the performance of the dam during the Kobe Earthquake. The analysis resulted in that large residual deformation and shear strain occurred at the shallow area of the upstream slope below the water level. The analysis was able to simulate the behavior and damage pattern of the dam, that is sliding deformation, during the Kobe Earthquake.

Department(s)

Civil, Architectural and Environmental Engineering

Meeting Name

4th International Conference on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics

Publisher

University of Missouri--Rolla

Document Version

Final Version

Rights

© 2001 University of Missouri--Rolla, All rights reserved.

Creative Commons Licensing

Creative Commons License
This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License.

Document Type

Article - Conference proceedings

File Type

text

Language

English

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Mar 26th, 12:00 AM Mar 31st, 12:00 AM

Numerical Simulation of Sliding of an Earth Dam During the 1995 Kobe Earthquake

San Diego, California

The Kobe Earthquake in Japan caused shallow sliding on the upstream slope below the water level of the Kitayama Dam. This paper briefly stated the results of post-earthquake surveys and tests of this earth dam. The FE model of the dam was prepared based on the detailed results of in-situ tests and laboratory material tests. The numerical analysis was performed by the effective stress analysis to simulate the performance of the dam during the Kobe Earthquake. The analysis resulted in that large residual deformation and shear strain occurred at the shallow area of the upstream slope below the water level. The analysis was able to simulate the behavior and damage pattern of the dam, that is sliding deformation, during the Kobe Earthquake.