Compressibility of an Isolated Spheroidal Cavity in an Isotropic Elastic Medium
Compressibility of an Isolated Spheroidal Cavity in an Isotropic Elastic Medium
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DOI:
10.1115/1.3169108
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发表时间:
1985-09
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影响因子:
--
通讯作者:
R. Zimmerman
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文献类型:
--
作者:
R. Zimmerman
A spheroidal cavity in an infinite, isotropic, elastic medium provides a useful model for the voids that are often present in rocks, ceramics, and porous metals. In its limiting forms, the spheroid can represent a sphere, an infinitely long cylinder, or a flat," penny-shaped" crack. An important property of such a void is its" pore compressibility," denoted here by Cpp, and defined as the fractional change in the volume of the cavity resulting from the application to its surface of a hydrostatic pressure of unit magnitude. Although the problem of the elastic field around a spheroidal cavity has been examined in the past [1-3], the focus of these studies has usually been on stress concentrations. Consequently, there are certain features applicable to pore compressibility that seem to have escaped notice. One is that the pore compressibility of a prolate spheroid, whose shape can range from a sphere to a cylinder, is for all intents and purposes a function only of the shear modulus, and nearly independent of the compressibility of the matrix material. Also, the asymptotic expression for the pore compressibility of an oblate spheroid of vanishingly small aspect ratio (the usual model for the penny-shaped crack) is actually highly accurate over nearly the entire range of oblate spheroid aspect ratios.