indent

Author: PrajaktaPMohite

cookbooks/melt_viscoplastic/melt_viscoplastic.prm

@@ -1,7 +1,7 @@
 # This cookbook illustrates how to combine time-dependent surface loading, free surface
-# deformation, a nonlinear viscoplastic rheology for the lithosphere and asthenosphere, and coupled 
+# deformation, a nonlinear viscoplastic rheology for the lithosphere and asthenosphere, and coupled
 # two-phase melting using the reactive fluid transport material model. The class of simulation
-# can be applied to tectonic settings where temporal changes in climate-driven surface 
+# can be applied to tectonic settings where temporal changes in climate-driven surface
 # loading has been proposed as a mechanism to explain variations in magmatism, such
 # as in Clerc et al. (2024), https://doi.org/10.1038/s41467-024-45890-z.
 
@@ -111,7 +111,7 @@ subsection Mesh refinement
   end
 end
 
-# Mesh deformation and free surface 
+# Mesh deformation and free surface
 # Advecting the free surface using a normal, rather than vertical,
 # projection. To reduce mesh instabilities and associated solver
 # issues when deformation becomes large, diffusion is applied to
@@ -125,7 +125,7 @@ subsection Mesh deformation
   end
 
   subsection Diffusion
-    # Diffusivity term. Increasing this value will result in a smoother 
+    # Diffusivity term. Increasing this value will result in a smoother
     # free surface and lower topography amplitudes.
     set Hillslope transport coefficient = 1.e-8
   end
@@ -137,7 +137,7 @@ end
 
 # Prescribe a fixed vertical traction on the top boundary
 # Adding parabolic ice load on top boundary at the middle of the model. The ice load is linearly
-# decreasing over time. 
+# decreasing over time.
 subsection Boundary traction model
   set Prescribed traction boundary indicators = top: function
 
@@ -156,7 +156,7 @@ subsection Melt settings
 end
 
 # The compositional fields represent:
-# 1-2. Fields representing porosity and peridotite, which are tracked with compositional fields. 
+# 1-2. Fields representing porosity and peridotite, which are tracked with compositional fields.
 # 3-6. Layers representing rock types, which are tracked with particles.
 
 subsection Compositional fields