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Title: Shear stress enhancement of void compaction

Technical Report ·
DOI:https://doi.org/10.2172/6740082· OSTI ID:6740082

Since the spherical model was successful in predicting the volumetric compaction behavior of both porous rocks and metals to a uniform pressure, the applicability of the spherical model to nonhydrostatic loading conditions was considered. Specifically, the spherical model is used to examine the influence of the presence of a shear stress on the volumetric compression of a porous solid. First the linear, elastic solution was obtained for a hollow sphere subject to homogeneous tractions on the outer boundary. Then, assuming that the matrix material is governed by the Drucker-Prager yield criterion, the elastic solution was used to derive an analytic expression for the onset of yield in the hollow sphere. The expression for the initial yield surface shows that the presence of a shear stress hastens the onset of yield in the sphere in comparison to a purely hydrostatic loading condition. This result agrees well with experimental data which show that, for porous solids, permanent crush-up begins at a lower mean stress under a nonhydrostatic loading than when the applied loading is a uniform pressure. At this point, due to difficulty in obtaining an analytic solution, a numerical scheme (finite element method) was used to extend the analysis of the hollow sphere problem into the elasto-plastic range. The spherical model results clearly exhibit the experimental finding that the presence of a shear stress tends to enhance the volumetric compaction of porous solids in comparison to a purely hydrostatic loading condition. For both a porous rock and metal sample, agreement between the spherical model and experimental results is excellent.

Research Organization:
Univ. of California, Berkeley, CA (United States)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
6740082
Report Number(s):
UCRL-13858
Country of Publication:
United States
Language:
English