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Introduction to Continuum Mechanics

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Transport Phenomena in Porous Media

Abstract

The mechanics of a deformable body treated here is based on Newton’s laws of motion and the laws of thermodynamics.

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Notes

  1. 1.

    In the second law (2.2) if we set \({ f}=\,{ 0}\) and solve the differential equation, we obtain \({ v}\,=\,\text{ constant}\) since m = { constant}, which suggests that the first law is included in the second law. This apparent contradiction results from the misinterpretation of the first law.

  2. 2.

    ‘Configuration’ is defined as an invertible continuous function that maps every material point \(X \in \mathfrak{B}\) to a point \({z}\) in a subset of the n-dimensional real number space \({\mathbb{R}}^{n}\). A time-dependent motion is considered; therefore the configuration is a function of the material point X and time t. The configuration at a given time t 0 is set as a reference configuration κ, and the point \({X} \in {\mathbb{R}}^{n}\) corresponding to a material point X is written as \({X}\,=\,\kappa (X),X\,=\,{\kappa }^{-1}({X})\) where κ − 1 is an inverse mapping of κ. The current configuration χ at time t maps X to \({x} \in {\mathbb{R}}^{n}\) as \({x}\,=\,\chi (X,t),X\,=\,{\chi }^{-1}({X}\!,t)\). The composite function \({\chi }_{\kappa }\,=\,\chi \circ {\kappa }^{-1}\) is introduced as \({x}\,=\,\chi ({\kappa }^{-1}({X}),t)\,=\,{\chi }_{\kappa }\,=\,\chi \circ {\kappa }^{-1}({X}\!,t)\,=\,{\chi }_{\kappa }({X}\!,t)\). The function χκ gives a mapping between the position vector \({X}\) in the reference configuration and the position vector \({x}\) in the current configuration. Since this formal procedure is complicated, the above simplified descriptions are employed.

  3. 3.

    If the gradient is used with respect to Eulerian coordinates with the basis {\({{e\!}}_{i}\}\), it is denoted as (2.14). If we explicitly explain the gradient with respect to the Eulerian system, it is denoted as \(\text{ grad} = {\Delta }_{x} ={ {e\!}}_{i} \dfrac{\partial \ } {\partial {x}_{i}}.\) If the gradient is operated with respect to Lagrangian coordinates {\({{E\!}}_{I}\}\), it is represented as \(\text{ Grad} = {\Delta }_{X} ={ {E\!}}_{I} \dfrac{\partial \ } {\partial {X}_{I}}.\)

  4. 4.

    Here we deal with a general case in which two coordinate systems may not be inertial systems. If both are inertial systems, \({Q}\) is time-independent as given by (2.4). Therefore, we have \({{x}}^{{_\ast}} = {Q}\,{x} + {V }t,\quad {{x}}_{0}^{{_\ast}} = {Q}\,{{x}}_{0} + {V }t\quad \Rightarrow \quad {u} ={ {x}}^{{_\ast}}-{{x}}_{0}^{{_\ast}} = {Q}({x}-{{x}}_{0}),\) which shows that the two-point vector \({u}\) is frame indifferent.

  5. 5.

    The convected derivatives of a vector \({v}\) are sometimes written as \({\delta }^{c}{v}/\delta t ={ \vartriangleleft \mathbf{v}},\:{\delta }_{c}{v}/\delta t ={ \vartriangleright \mathbf{v}}\). For the second-order tensor \({T}\) these are \({\delta }^{cc}{T}/\delta t ={ \vartriangleleft \mathbf{T}},\:{\delta }_{cc}{T}/\delta t ={ \vartriangleright \mathbf{T}}\).

  6. 6.

    The inner product of the second-order tensors \({A},\ {B}\) is introduced by \({A} : {B} = \mathrm{tr}\,({{A}}^{T}{B}) = {A}_{\mathit{ij}}\,{B}_{\mathit{ij}}\). \({A}\) and \({B}\) are orthogonal if \({A} : {B} = 0\).

  7. 7.

    The definition of the δ-function is given by \({\int \nolimits \nolimits }_{\Omega }dy\,\delta (y - x)f(y) = f(x)\).

  8. 8.

    Leibnitz rule: If we have an integral of a continuous function f such as

    $$\qquad \phi (x) ={ \int \nolimits \nolimits }_{{h}_{0}(x)}^{{h}_{1}(x)}f(x,\xi )\,d\xi,$$

    and if h 1(x) and h 0(x) are continuous on R = { (x, ξ) :  a ≤ x ≤ b,  c ≤ ξ ≤ d }, then

    $$\qquad \frac{d\phi (x)} {dx} = f\left (x,{h}_{1}(x)\right )\frac{d{h}_{1}(x)} {dx} - f\left (x,{h}_{0}(x)\right )\frac{d{h}_{0}(x)} {dx} +{ \int \nolimits \nolimits }_{{h}_{0}(x)}^{{h}_{1}(x)}\frac{\partial f(x,\xi )} {\partial x} \,d\xi $$

    (see, e.g., Protter and Morrey 1977, pp. 284).

  9. 9.

    Note that the differentiation implies \({\overline{E}}^{(k)}(k\tau ) = \dfrac{{d}^{k}\overline{E}(k\tau )} {d{(k\tau )}^{k}}\). Others are the same.

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© 2012 Springer-Verlag Berlin Heidelberg

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Ichikawa, Y., Selvadurai, A.P.S. (2012). Introduction to Continuum Mechanics. In: Transport Phenomena in Porous Media. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-25333-1_2

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  • DOI: https://doi.org/10.1007/978-3-642-25333-1_2

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