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- W1217329905 abstract "This chapter provides an overview of linear poroelasticity. It is a theory that includes the coupling between linear diffusion of a mobile species and the stress and deformation of a linear elasticporous solid. This theory is widely applied not only to soils and rock masses infiltrated by groundwater but also to coupling of fluid flow and deformation in biological materials and diffusion of hydrogen in metals. Although departures from linear behavior are common in actual materials, linear poroelasticity is an improvement over idealizations that neglect either diffusion or deformation entirely. Because parameters describing nonlinear material behavior are difficult to obtain with accuracy, poroelasticity often offers a more practical approach than complex, nonlinear models. The drained elastic constants and two parameters are needed to characterize a linear poroelastic solid. Ideally, the drained elastic constants is measured on a saturated sample deformed very slowly so that no pore pressure changes are induced by fluid flow. In practice, however, the drained elastic constants are often assumed to be equal to the values obtained on dry samples. Furthermore, the insight gained from linear poroelasticity is valuable for interpreting more complex models." @default.
- W1217329905 created "2016-06-24" @default.
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- W1217329905 date "2001-01-01" @default.
- W1217329905 modified "2023-10-16" @default.
- W1217329905 title "Linear Poroelasticity" @default.
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- W1217329905 doi "https://doi.org/10.1016/b978-012443341-0/50113-7" @default.
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