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Why the stress ratios are constant in the residual state of sheared granular materials regardless of the materials?(I142-012)(abs.)
SAKAGUCHI Hide
itemdescription
TitleWhy the stress ratios are constant in the residual state of sheared granular materials regardless of the materials?(I142-012)(abs.)
AuthorsSAKAGUCHI Hide
Data nameAbstracts, Japan Geoscience Union Meeting (CD-ROM)
Volume2006
PageI142-012
Year2006
PublisherJapan Geoscience Union
LanguageJA, EN
@idhttps://gbank.gsj.jp/ld/resource/geolis/200660294