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Fix typos
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include/aspect/plugins.h

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@@ -217,7 +217,7 @@ namespace aspect
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/**
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* A function that is called at the beginning of each time step,
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* calling the update function of the individual heating models.
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* calling the update function of the individual plugins.
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*/
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void
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update () override;

source/boundary_convective_heating/interface.cc

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@@ -319,7 +319,7 @@ namespace aspect
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"For heat transfer coefficient --> zero, the boundary approaches "
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"insulating (Neumann) behaviour; "
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"For heat transfer coefficient --> infinity, the boundary approaches "
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"a prescribed-temperature (Dirichlet) condition."
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"a prescribed-temperature (Dirichlet) condition. "
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"The unit of the heat transfer coefficient is \\si{\\watt\\per\\meter\\squared\\per\\kelvin}."
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"At the moment, this list can only have one entry. \n\n"
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"The following heat transfer coefficient models are available:\n\n"
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"use in your model."
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"\n\n"
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"This parameter only describes which boundaries have a fixed "
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"convective flux (i.e. Robin boundarry condictions), but not what "
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"convective flux (i.e. Robin boundary condictions), but not what "
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"conditions should hold on these boundaries. "
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"The latter piece of information needs to be "
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"implemented in a plugin in the BoundaryConvectiveHeating "

source/geometry_model/chunk.cc

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@@ -944,8 +944,8 @@ namespace aspect
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"The dimensions of the model are specified by parameters "
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"of the following form: "
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"Chunk (minimum || maximum) (longitude || latitude): "
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"edges of geographical quadrangle (in degrees)"
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"Chunk (inner || outer) radius: Radii at bottom and top of chunk"
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"edges of geographical quadrangle (in degrees). "
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"Chunk (inner || outer) radius: Radii at bottom and top of chunk. "
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"(Longitude || Latitude || Radius) repetitions: "
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"number of cells in each coordinate direction."
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"\n\n"

source/geometry_model/two_merged_boxes.cc

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@@ -639,7 +639,7 @@ namespace aspect
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"The extent of the box in each coordinate direction "
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"is set in the parameter file. This geometry model labels its "
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"sides with 2*dim+2*(dim-1) boundary indicators: in 2d, boundary indicators 0 through 3 "
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"denote the left, right, bottom and top boundaries, while indicators"
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"denote the left, right, bottom and top boundaries, while indicators "
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"4 and 5 denote the upper part of the left and right vertical boundary, "
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"respectively. In 3d, boundary "
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"indicators 0 through 5 indicate left, right, front, back, bottom "

source/simulator/parameters.cc

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

source/time_stepping/repeat_on_cutback.cc

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@@ -108,7 +108,7 @@ namespace aspect
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"shrinks by more than a user-controlled factor. In that situation, the previous "
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"time step will be repeated with a smaller step size.\n"
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"A large reduction in time step size typically happens when velocities change "
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"abruptly. Repeating the time step ensure properly resolving this event. It is "
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"abruptly. Repeating the time step ensures properly resolving this event. It is "
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"useful to consider setting the \"Maximum relative increase in time step\" option "
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"to avoid repeatedly repeating every other time step.")
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}

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