Calculates the Hantush-Jacob solution (drawdown) in the Laplace domain
hantush_jacob_WF_LT(p, arg1, ...)
| p | Laplace parameter |
|---|---|
| arg1 | Beta parameter. The beta parameter is defined as $$\beta = \frac{r}{4} \sqrt{\frac{k_{h}^{'}S_{s}^{'}}{TS}}$$ where \(T\) and \(S\) are the transmissivity and storage coefficient of the aquifer, and \(k_{h}^{'}\) and \(S_{s}^{'}\) are the vertical hydraulic conductivity and the Storage coefficient of the aquitard respectively. |
| ... | Additional parameters |
A numeric vector with the calculated drawdown in the Laplace domain
Hantush, M. S. Flow to wells in aquifers separated by a semipervious layer. Journal of Geophysical Research, 1967, 72, 1709.
Other hantush_jacob functions: hantush_jacob_WF_LT_dlogt,
hantush_jacob_calculate_parameters,
hantush_jacob_solution_dlogt,
hantush_jacob_solution_initial,
hantush_jacob_solution,
hantush_jacob_well_function
#> [1] 0.8552223