Description Usage Arguments Value Author(s) References See Also Examples
View source: R/hantush_jacob_utilities.R
Calculates the Hantush-Jacob solution (drawdown) in the Laplace domain
1 | hantush_jacob_WF_LT(p, arg1, ...)
|
p |
Laplace parameter |
arg1 |
Beta parameter. The beta parameter is defined as β = \frac{r}{4} √{\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
Oscar Garcia-Cabrejo khaors@gmail.com
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 2 3 4 | p <- 0.5
beta <- 0.5
res <- hantush_jacob_WF_LT(p, beta)
print(res)
|
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.