1989
DOI: 10.1007/bf01175798
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Integral formulation and fundamental solutions of dynamic poroelasticity and thermoelasticity

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Cited by 88 publications
(36 citation statements)
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“…Since there is an analogy between the steady-state theories of thermoelasticity and poroelasticity (see e.g. Manolis and Beskos [30]), the present results are applicable in the latter case too. In this first-step analysis, the effect of friction is ignored and the indentor is assumed to be non-conducting.…”
Section: Introductionmentioning
confidence: 72%
See 1 more Smart Citation
“…Since there is an analogy between the steady-state theories of thermoelasticity and poroelasticity (see e.g. Manolis and Beskos [30]), the present results are applicable in the latter case too. In this first-step analysis, the effect of friction is ignored and the indentor is assumed to be non-conducting.…”
Section: Introductionmentioning
confidence: 72%
“…The governing equations of the problem according to the linear coupled thermoelastodynamic theory [29,30,32] will now be written. With respect to a fixed Cartesian…”
Section: Problem Statementmentioning
confidence: 99%
“…Upon close inspection of their paper [1], the authors noticed a number of errors that have to be corrected. First of all, the coefficients ax2 and a2~ in equation (13) are not equal.…”
Section: Correctionsmentioning
confidence: 99%
“…The Green's tensors have already been derived by several authors using either Helmholtz decomposition or the so-called Kupradze's method (Burridge & Vargas, 1979;Norris, 1985;Bonnet, 1987;Manolis & Beskos, 1989;Philippacopoulos, 1998;Sahay, 2001), and considering different sources. In the paper by Burridge & Vargas (1979) only a force applied to the total medium (fluid and solid) is included, i.e., a vector containing three sources (components).…”
Section: Introductionmentioning
confidence: 99%
“…In the paper by Burridge & Vargas (1979) only a force applied to the total medium (fluid and solid) is included, i.e., a vector containing three sources (components). Other authors considered only a force applied to the solid of the porous medium (Norris, 1985;Philippacopoulos, 1998), which implies also three sources, while Manolis & Beskos (1989) included forces applied to both the solid and fluid, i.e., six sources. Sahay (2001) also included six sources but with a different physical meaning, i.e., one force associated with the inphase fluid-solid motion (applied to the center of mass of the porous medium), and one with the relative motion of the fluid and solid.…”
Section: Introductionmentioning
confidence: 99%