Question: please i need help with the code and not an explanation. thank you Use Liebeman method ( also known as Gauss Siedel method ) with

please i need help with the code and not an explanation. thank you
Use Liebeman method (also known as Gauss Siedel method) with over relaxation to determine the flow in the aquifer shown in figure 1, with the following properties: hydraulic conductivity k=10m? day, groundwater recharge N=0mm? day, thickness of the aquifer D=50m.
The boundary conditions of the aquifer are
BOUNDARY 1: no-flow near the mountains;
BOUNDARY 2: linear from 100 m (near mountains) to 0 m (near sea);
BOUNDARY 3: constant seawater level of 0 m ;
BOUNDARY 4: no-flow.
Figure 1. Aquifer with boundary conditions
Run the model for two possible solutions:
\table[[Solution I:,Solution II:],[Initial estimate head =50m,- Initial estimate head=50m],[Convergence-criterion=1m,- Convergence-criterion=0.01 m],[Number of iterations =13,- Number of iterations=74],[Head 1=29,17m,- Head 1=20,67m
please i need help with the code and not an

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