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Residual undrained shear strength, su, of granular soils is often estimated from back analysis of post-earthquake geometry of embankments. In these analyses soil behavior is usually assumed to be inherently isotropic although saturated sandy soils exhibit strong inherent anisotropy under undrained loading. This paper presents back-analyses of two case histories of undrained instability of embankments observed during the Magnitude (Japanese Meteorological Agency) 7.8 (MJMA 7.8) Kushiro-Oki Earthquake of January 15, 1993 considering inherently anisotropic soil behavior. The residual undrained shear strengths obtained from these analyses were then compared with the corresponding estimates from conventional back-analyses which assume inherently isotropic soil behavior.
Residual undrained shear strength, su, of granular soils is often estimated from back analysis of post-earthquake geometry of embankments. In these analyses soil behavior is usually assumed to be inherently isotropic although saturated sandy soils exhibit strong inherent anisotropy under undrained loading. This paper presents back-analyses of two case histories of undrained instability of embankments observed during the Magnitude (Japanese Meteorological Agency) 7.8 (MJMA 7.8) Kushiro-Oki Earthquake of January 15, 1993 considering inherently anisotropic soil behavior. The residual undrained shear strengths obtained from these analyses were then compared with the corresponding estimates from conventional back-analyses which assume inherently isotropic soil behavior.
Anisotropic Undrained Back-Analysis of Embankments
GeoShanghai International Conference 2006 ; 2006 ; Shanghai, China
Advances in Earth Structures ; 225-230
2006-05-11
Conference paper
Electronic Resource
English
Anisotropic Undrained Back-Analysis of Embankments
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