1970
DOI: 10.1016/0020-7683(70)90055-7
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An isotropic frictional theory for a granular medium with or without cohesion

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Cited by 11 publications
(1 citation statement)
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“…Neither of the results quoted above are applicable since the first requires a differentiable yield function and the second a unique correspondence between the tensors of stress and strain rate or their deviators. Moreover, coincidence does not hold for an isotropic frictional material [4], which obeys the verbal hypotheses upon which coincidence for the Tresca material is generally taken.In Sec. 1 a pictorial description of the rigid perfectly plastic Tresca material is given and it is explained why coincidence does not hold for the conceptually similar frictional material.…”
mentioning
confidence: 99%
“…Neither of the results quoted above are applicable since the first requires a differentiable yield function and the second a unique correspondence between the tensors of stress and strain rate or their deviators. Moreover, coincidence does not hold for an isotropic frictional material [4], which obeys the verbal hypotheses upon which coincidence for the Tresca material is generally taken.In Sec. 1 a pictorial description of the rigid perfectly plastic Tresca material is given and it is explained why coincidence does not hold for the conceptually similar frictional material.…”
mentioning
confidence: 99%