Directly searching method for slip plane and its influential factors based on critical state of slope

In order to determine the slip plane of slope directly by the calculation results of strength reduction method, and analyze the influential factors of slope stability, a numerical model was established in plane strain mode by FLAC3D for homogeneous soil slope, whose parameters were reduced until the...

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Published inJournal of Central South University of Technology. Science & technology of mining and metallurgy Vol. 16; no. 1; pp. 131 - 135
Main Authors Lin, Hang, Cao, Ping, Gong, Feng-qiang, Li, Jiang-teng, Gui, Yi-lin
Format Journal Article
LanguageEnglish
Published Heidelberg Central South University 01.02.2009
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ISSN1005-9784
1993-0666
DOI10.1007/s11771-009-0022-6

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Summary:In order to determine the slip plane of slope directly by the calculation results of strength reduction method, and analyze the influential factors of slope stability, a numerical model was established in plane strain mode by FLAC3D for homogeneous soil slope, whose parameters were reduced until the slope reached the critical state. Then FISH program was used to get the location data of slip plane from displacement contour lines. Furthermore, the method to determine multiple slip planes was also proposed by setting different heights of elastic areas. The influential factors for the stability were analyzed, including cohesion, internal friction angle, and tensile strength. The calculation results show that with the increase of cohesion, failure mode of slope changes from shallow slipping to the deep slipping, while inclination of slip plane becomes slower and slipping volume becomes larger; with the increase of friction angle, failure mode of slope changes from deep slipping to shallow slipping, while slip plane becomes steeper and upper border of slip plane comes closer to the vertex of slope; the safety factor increases little and slip plane goes far away from vertex of slope with the increase of tensile strength.
ISSN:1005-9784
1993-0666
DOI:10.1007/s11771-009-0022-6