Calculates the Hantush-Jacob solution (drawdown) in the Laplace domain

hantush_jacob_WF_LT(p, arg1, ...)

Arguments

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

Value

A numeric vector with the calculated drawdown in the Laplace domain

References

Hantush, M. S. Flow to wells in aquifers separated by a semipervious layer. Journal of Geophysical Research, 1967, 72, 1709.

See also

Examples

p <- 0.5 beta <- 0.5 res <- hantush_jacob_WF_LT(p, beta) print(res)
#> [1] 0.8552223