[cleanup] Corrected further inconsistent spelling instances

lecture/efm/1p2c_2p_2p2c/description/timescale_solution.tex

@@ -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}

lecture/efm/1p2cvs2p/exercise1.input

@@ -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 [-]
 ########
 
 [Boundary]