作者: G. Hocking
DOI: 10.1016/0148-9062(76)91697-1
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摘要: A simple rule to distinguish between single and double plane sliding of tetrahedral wedges, assuming only body forces hydrostatic are acting, is presented. This differs from that given by panet, who assumed the analysis was independent orientation slope face for case; this assumption shown be incorrect. The distinction important; if down line intersection always assumed, then stability wedge will overestimated cases in which a actually occurs. /TRRL/