pastas.recharge.Berendrecht#
- class pastas.recharge.Berendrecht#
Nonlinear recharge to the groundwater.
Calculated according to Berendrecht et al. [2006].
Notes
Note that the preferred unit of the precipitation and evaporation is mm/d. The water balance for the unsaturated zone reservoir is written as:
\[\begin{split}\\frac{dS_e}{dt} = \\frac{1}{D_e}(f_iP - E_a - R)\end{split}\]where the recharge is calculated as:
\[\begin{split}R(S_e) = K_sS_e^\\lambda(1-(1-S_e^{1/m})^m)^2\end{split}\]For a detailed description of the recharge model and parameters we refer to the original publication.
Methods#
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Get initial parameters and bounds for the Berendrecht recharge model. |
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Simulate the recharge flux. |
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Calculate recharge flux sped up with numba. |
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Get the water balance for the Berendrecht recharge model. |