@@ -1131,7 +1131,7 @@ namespace aspect
11311131 prm.declare_entry (" List of compositional fields with disabled boundary entropy viscosity" , " " ,
11321132 Patterns::List (Patterns::Anything ()),
11331133 " Select for which compositional fields to skip the entropy viscosity "
1134- " stabilization at dirichlet boundaries. This is "
1134+ " stabilization at Dirichlet boundaries. This is "
11351135 " only advisable for compositional fields "
11361136 " that have intrinsic physical diffusion terms, otherwise "
11371137 " oscillations may develop. The parameter should contain a list of "
@@ -1154,7 +1154,7 @@ namespace aspect
11541154 " Rather, the paper always uses 2 as the exponent in the definition "
11551155 " of the entropy, following equation (15) of the paper. The full "
11561156 " approach is discussed in \\ cite{guermond:etal:2011}.) Note that this is not the "
1157- " thermal expansion coefficient, also commonly referred to as $\\ alpha$."
1157+ " thermal expansion coefficient, also commonly referred to as $\\ alpha$. "
11581158 " Units: None." );
11591159 prm.declare_entry (" cR" , " 0.11" ,
11601160 Patterns::List (Patterns::Double (0 .)),
@@ -1341,8 +1341,8 @@ namespace aspect
13411341 " determine the equation of state, rheology, and reactions."
13421342 " \n "
13431343 " * ``stress'': This type of field represents stress in the material. "
1344- " Whether the fields represents a scalar stress invariant or "
1345- " tensor components , and which type of stress is represented "
1344+ " Whether the field represents a scalar stress invariant or a "
1345+ " tensor component , and which type of stress is represented "
13461346 " depends on the interpretation of the material model."
13471347 " \n "
13481348 " * ``strain'': This type of field represents accumulated strain. "
@@ -1443,8 +1443,8 @@ namespace aspect
14431443 " field as mentioned in Section~\\ ref{sec:methods:compositional-fields}, except that it is "
14441444 " advected with the Darcy velocity instead of the solid velocity. This method "
14451445 " requires there to be a compositional field named porosity that is advected "
1446- " the darcy field method. We calculate the fluid velocity $u_f$ using an "
1447- " approximation of Darcy's Law: $u_f = u_s - K_D / \\ phi * (rho_s * g - rho_f * g)$."
1446+ " with the darcy field method. We calculate the fluid velocity $u_f$ using an "
1447+ " approximation of Darcy's Law: $u_f = u_s - K_D / \\ phi * (\\ rho_s * g - \\ rho_f * g)$."
14481448 " \n "
14491449 " * ``prescribed field'': The value of these fields is determined "
14501450 " in each time step from the material model. If a compositional field is "
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