By J. W. Rudnicki (auth.), A. P. S. Selvadurai (eds.)
ISBN-10: 9048145139
ISBN-13: 9789048145133
ISBN-10: 9401586985
ISBN-13: 9789401586986
In Mechanics of Poroelastic Media the classical idea of poroelasticity built via Biot is constructed and prolonged to the examine of difficulties in geomechanics, biomechanics, environmental mechanics and fabrics technology. The contributions are grouped into sections overlaying constitutive modelling, analytical elements, numerical modelling, and functions to difficulties. The purposes of the classical conception of poroelasticity to a much wider type of difficulties can be of specific curiosity. The textual content is a typical reference for researchers drawn to constructing mathematical types of poroelasticity in geoenvironmental mechanics, and within the software of complicated theories of poroelastic biomaterials to the mechanics of biomaterials.
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Extra info for Mechanics of Poroelastic Media
Sample text
H permeable faces_ " . I' 1 . 0° 10·\ :' . h imperme:able (aces. 10· - , mode I ... cnsi~.. a,,,, Figure 9: The non·dimenslonahsed mode I stress intensity factor (for v = 0 1, N" = 0 -i) vel'sus tlllle, for the full solution (3,23), d ot. ted line, the small tllne solution, dashed hne , and the large time solution, solid line ' O"~I~~~~~~~~~~~~~~~~~~--~~~ 1004 10" 10] 10' IG' . 3, I/~ = 0 I) versus time, for the full solution, dotted line, the small time solution, di\shed line, and the large time solu· tion , sohd line.
Proc. U. S. , University of Nevada Reno, pp. 274-282. Simons, D. A. (1979), The analysis of propagating slip zones in porous elastic media, in R. ), Fracture Mechanics, Proceedings oJthe symposium in applied mathematics oj AMS and SIAM, SIAMAMS, New York, pp. 153-169. Wang, C-Y. and Lin, W. (1978), Constitution of the San Andreas fault zone at depth, Geophysical Research Letters 5, 741-744. Wesson, R. L. (1981), Interpretation of changes in water level accompanying fault creep and implications for earthquake prediction, J.
Solids, 25, 99-115 Skempton A. 1954, "The pore pressure coefficients A and B," Geoteehnique,4, 143147 A. e. e. e. e. , m = Poc:, and the following relations are used in the text. 3(vu - v) Q 2GB 2(1 - 2v)(1 + vu)2 a = B(1 _ 2v)(1 + vu )' = 9(vu - v)(1 - 2vu) , I-v 11 _ (1 - vu ) = 1- 2v' ,1Iu = 2( Vu - _ (1 - v) ) , 11 = 2{ ), V Vu - v (A 1) . 3) 1 No = "2(1 - 27]). (AA) 45 B. 5) (~+ i)~ the subscripts +(-) are used to denote functions analytic in the upper (lower) halves of the complex ~ plane.
Mechanics of Poroelastic Media by J. W. Rudnicki (auth.), A. P. S. Selvadurai (eds.)
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