Commit 93f053c0 authored by Mathis Kelm's avatar Mathis Kelm
Browse files

[cleanup] Corrected further inconsistent spelling instances

parent d029dfe6
......@@ -169,7 +169,7 @@ Alltogether this leads to 15 unknowns and 13 equations plus the two transport eq
as long as $ 0 < S_\alpha < 1$.
\item Only wetting phase is present: The mass fraction of, e.g., N$_2$ in the wetting phase $X^n_l$ is used,
as long as the maximum mass fraction is not exceeded ($X^n_l<X^n_{l,max}$)
\item Only nonwetting phase is present: The mass fraction of, e.g., water in the non-wetting phase, $X^w_g$, is used,
\item Only nonwetting phase is present: The mass fraction of, e.g., water in the nonwetting phase, $X^w_g$, is used,
as long as the maximum mass fraction is not exceeded ($X^w_g<X^w_{g,max}$)
\end{itemize}
......
......@@ -24,9 +24,9 @@ FineBrooksCoreyEntryPressure = 400 # entry pressure for the Brooks-Core
CoarseBrooksCoreyLambda = 2.0 # pore size distribution parameter for the Brooks-Corey capillary pressure - saturation relationship in the coarse soil [-]
CoarseBrooksCoreyEntryPressure = 200 # entry pressure for the Brooks-Corey capillary pressure - saturation relationship in the coarse soil [Pa]
FineResidualSaturationWetting = 0.05 # residual saturation of the wetting phase in the fine soil [-]
FineResidualSaturationNonWetting = 0.3 # residual saturation of the nonwetting phase in the fine soil [-]
FineResidualSaturationNonwetting = 0.3 # residual saturation of the nonwetting phase in the fine soil [-]
CoarseResidualSaturationWetting = 0.05 # residual saturation of the wetting phase in the coarse soil [-]
CoarseResidualSaturationNonWetting = 0.1 # residual saturation of the nonwetting phase in the coarse soil [-]
CoarseResidualSaturationNonwetting = 0.1 # residual saturation of the nonwetting phase in the coarse soil [-]
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[Boundary]
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