From: Wolfgang Bangerth Date: Mon, 7 Aug 2023 10:13:14 +0000 (-0600) Subject: Fix quotation issue. X-Git-Url: https://gitweb.dealii.org/cgi-bin/gitweb.cgi?a=commitdiff_plain;h=refs%2Fpull%2F157%2Fhead;p=code-gallery.git Fix quotation issue. --- diff --git a/Nonlinear_PoroViscoelasticity/nonlinear-poro-viscoelasticity.cc b/Nonlinear_PoroViscoelasticity/nonlinear-poro-viscoelasticity.cc index 522abd2..aba1113 100644 --- a/Nonlinear_PoroViscoelasticity/nonlinear-poro-viscoelasticity.cc +++ b/Nonlinear_PoroViscoelasticity/nonlinear-poro-viscoelasticity.cc @@ -702,9 +702,9 @@ namespace NonLinearPoroViscoElasticity // @sect3{Constitutive equation for the solid component of the biphasic material} //@sect4{Base class: generic hyperelastic material} -// The ``extra" Kirchhoff stress in the solid component is the sum of isochoric -// and a volumetric part. -// $\mathbf{\tau} = \mathbf{\tau}_E^{(\bullet)} + \mathbf{\tau}^{\textrm{vol}}$ +// The "extra" Kirchhoff stress in the solid component is the sum of isochoric +// and a volumetric part: +// $\mathbf{\tau} = \mathbf{\tau}_E^{(\bullet)} + \mathbf{\tau}^{\textrm{vol}}$. // The deviatoric part changes depending on the type of material model selected: // Neo-Hooken hyperelasticity, Ogden hyperelasticiy, // or a single-mode finite viscoelasticity based on the Ogden hyperelastic model. @@ -713,7 +713,7 @@ namespace NonLinearPoroViscoElasticity // We define here the volumetric component, which depends on the // extension function $U(J_S)$ selected, and in this case is the same for all models. // We use the function proposed by -// Ehlers & Eipper 1999 doi:10.1023/A:1006565509095 +// Ehlers & Eipper 1999 doi:10.1023/A:1006565509095. // We also define some public functions to access and update the internal variables. template > class Material_Hyperelastic @@ -1324,7 +1324,7 @@ namespace NonLinearPoroViscoElasticity // for storing data at the quadrature points. Here each quadrature point // holds a pointer to a material description. Thus, different material models // can be used in different regions of the domain. Among other data, we -// choose to store the ``extra" Kirchhoff stress $\boldsymbol{\tau}_E$ and +// choose to store the "extra" Kirchhoff stress $\boldsymbol{\tau}_E$ and // the dissipation values $\mathcal{D}_p$ and $\mathcal{D}_v$. template > //double> class PointHistory