3. Continuous equations#
3.1. Mechanics: conservation of momentum#
We note \(\sigma\) the Cauchy stress tensor and \(s\) the second (symmetric) Piola-Kirchhoff tensor.
We denote \(P\) as the \({x}_{0}={x}_{S}(0)\to {x}_{S}({x}_{0},t)\) transformation gradient.
\(P=\frac{\partial {x}_{S}({x}_{0},t)}{\partial {x}_{0}}\)
We have: \(s=\text{det}P\text{.}{P}^{-1}\text{.}\sigma \text{.}{P}^{-T}\).
The mechanical balance equations are written in configuration \({\Omega }_{0}\):
\({\text{Div}}_{0}(P\text{.}s)+r{F}^{m}=0\)
We noted \({\text{Div}}_{0}\) as the divergence operator with respect to the \({x}_{0}\) space variables in the \({\Omega }_{0}\) configuration.
Insofar as we hypothesize small displacements and small deformations of the skeleton, this equation can be approximated by:
\(\text{Div}\sigma +r{F}^{m}=0\) eq 3.1-1
We will see later that we are still adopting the \(\sigma =\sigma \text{'}+{\sigma }_{p}I\) decomposition, where \(\sigma \text{'}\) refers to the effective constraint. It is therefore up to the module for integrating balance equations to do the sum: \(\sigma =\sigma \text{'}+{\sigma }_{p}I\).
3.2. Hydraulics: mass conservation#
The Eulerian writing for the conservation of fluid mass for the constituent \(c\) is written:
\(\frac{{d}^{\mathrm{fl}}}{\mathrm{dt}}\int {}_{\Omega }\text{}\sum _{p}{\rho }_{c}^{p}\phi {S}^{p}d\Omega =0\)
We can then apply [éq 2.3-1] by taking: \({a}_{s}=0\) and \({{a}^{m}}_{c}^{p}=1\) and [éq 2.3-3] will give:
\(\sum _{p}\frac{{d}^{s}{\rho }_{c}^{p}\phi {S}^{p}}{\mathrm{dt}}+\sum _{p}\text{Div}({w}_{c}^{p})=0\)
Using the definition of mass inputs [éq 2.2.2.3-3], the definition of Lagrangian flows [éq2.2.2.3-2] we find the Lagrangian form of fluid mass conservation:
\(\{\begin{array}{}\dot{{m}_{1}}+{\text{Div}}_{0}({M}_{1})=0\\ \dot{{m}_{2}}+{\text{Div}}_{0}({M}_{2})=0\end{array}\) eq 3.2-1
3.3. Energy equation#
For thermodynamic functions, we systematically adopt a decomposition of the [éq2.3-1] type. This corresponds to the fact that the different energies all have a part carried by the solid and a part carried by the fluids. The part carried by the solid is characterized by a volume density while the parts carried by the fluid are characterized by mass densities, as we showed in paragraph [§2.3].
Total internet energy: \(E=\int {}_{\Omega }\text{}({e}_{s}+\sum _{p,c}{\rho }_{c}^{p}\phi {S}^{p}{{e}^{m}}_{c}^{p})d\Omega\) eq 3.3.1
Total entropy: \(S=\int {}_{\Omega }\text{}({s}_{s}+\sum _{p,c}{\rho }_{c}^{p}\phi {S}^{p}{{s}^{m}}_{c}^{p})d\Omega\) eq 3.3.2
Total enthalpy: \(H=\int {}_{\Omega }\text{}({h}_{s}+\sum _{p,c}{\rho }_{c}^{p}\phi {S}^{p}{{h}^{m}}_{c}^{p})d\Omega\) eq 3.3.3
Free energy: \(\{\begin{array}{}\Psi =E-TS\\ {\Psi }_{s}={e}_{s}-{\text{Ts}}_{s}\\ {{\Psi }^{m}}_{c}^{p}={{e}^{m}}_{c}^{p}-T{{s}^{m}}_{c}^{p}\end{array}\) eq 3.3.4
Free enthalpy: \(\{\begin{array}{}G=H-TS\\ {g}_{s}={h}_{s}-T{s}_{s}\\ {{g}^{m}}_{c}^{p}={{h}^{m}}_{c}^{p}-T{{s}^{m}}_{c}^{p}\end{array}\) eq 3.3.5
Finally, by noting \(\dot{Q}(\Omega )\) the heat rate received by a volume \(\Omega\), we have by definition:
\(\dot{Q}(\Omega )=\underset{\partial \Omega }{\int }q\text{.}nd\Gamma +\underset{\Omega }{\int }\Thetad \Omega\) eq 3.3.6
Finally, we recall that the enthalpy of fluids is calculated by the formula:
\(h=e+\frac{p}{\rho }\) eq 3.3.7
3.3.1. The first principle#
With the definitions given above, it is written:
\(-\sum _{p,c}\text{Div}\left({{h}^{m}}_{c}^{p}{\mathrm{M}}_{c}^{p}\right)+\mathrm{\sigma }\mathrm{:}\dot{\mathrm{\epsilon }}+\sum _{p,c}{\mathrm{M}}_{c}^{p}\text{.}{\mathrm{F}}^{m}+\mathrm{\Theta }-\text{Div}q=0\) eq 3.3.1-1
This writing corresponds to equation (22) in chapter III -2-3 of [bib1], in which we neglected inertia terms. For homogeneous media, it corresponds to equation (31) in paragraph IV-3-2 of [bib3].
3.3.2. The second principle#
Its fairly well known form is:
\(\dot{s}+\sum _{p,c}\text{Div}({{s}^{m}}_{c}^{p}{M}_{c}^{p})+\text{Div}(\frac{q}{T})-\frac{\Theta }{T}\ge 0\) eq 3.3.2-1
Using the classical thermodynamic considerations [bib1] linked to the introduction of free enthalpy [éq 3.3.5], we show that we must necessarily have:
\(\sigma -\frac{\partial \Psi }{\partial \varepsilon }=0\) eq 3.3.2-2
\({{g}^{m}}_{c}^{p}-\frac{\partial \Psi }{\partial {m}_{c}^{p}}=0\) eq 3.3.2-3
\(s+\frac{\partial \Psi }{\partial T}=0\) eq 3.3.2-4
3.3.3. Energy equation#
Quite often, it is considered that, since the transformations are reversible, the second principle ultimately provides equality. In addition, in [éq 3.3.2-1] the unknown temperature \(T\) is replaced by a constant value called the reference temperature. It is finally a linearization of [éq 3.3.2-1] justified if the temperature variations are « small ». Note that the transport term \(\sum _{p,c}\text{Div}({{s}^{m}}_{c}^{p}{M}_{c}^{p})\) complicates the treatment of nonlinearity due to the presence of temperature in the denominator of the other terms in [éq 3.3.2-1].
We work in enthalpy in order to overcome this difficulty. We start from the equation of the first principle [éq 3.3.1-1] into which we inject the equations [éq 3.3.2-2], [], [éq 3.3.2-3], [éq 3.3.2-4], and the definition of free enthalpy [éq 3.3-5] into which we obtain:
\(T\dot{s}+\sum _{p,c}({{h}^{m}}_{c}^{p}\dot{{m}_{c}^{p}}-T{{s}^{m}}_{c}^{p}\dot{{m}_{c}^{p}})=-\sum _{p,c}\text{Div}({{h}^{m}}_{c}^{p}{M}_{c}^{p})+\sum _{p,c}{M}_{c}^{p}\text{.}{F}^{m}+\Theta -\text{Div}q\) eq 3.3.3-1
We then ask:
\(\deltaq \text{'}=T\deltas -T\sum _{p,c}{s}^{{m}_{c}^{p}}\delta {m}_{c}^{p}\) eq 3.3.3-2
The quantity \(Q\text{'}\) has the dimension of one energy per unit volume. It represents the heat received by the system in a transformation for which there is no heat input by entering a fluid having an enthalpy. Although \(\deltaq \text{'}\) is not an exact differential, we take this quantity as a state variable.
Finally, the energy equation adopted has the following form:
\(\sum _{p,c}{{h}^{m}}_{c}^{p}\dot{{m}_{c}^{p}}+\dot{Q\text{'}}+\sum _{p,c}\text{Div}({{h}^{m}}_{c}^{p}{M}_{c}^{p})+\text{Div}q-\sum _{p,c}{M}_{c}^{p}\text{.}{F}^{m}=\Theta\) eq 3.3.3-3