hantush_jacob_well_function: hantush_jacob_well_function

In khaors/pumpingtest: R Package for the analysis and evaluation of pumping tests

Description

Well function of the Hantush-Jacob model

Usage

hantush_jacob_well_function(td, par)

Arguments

td	Dimensionless time
par	List with the beta parameter and the coefficients used in the Stehfest inversion approach. 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.

Value

The value of the dimensionless drawdown of the Hantush-Jacob model

Author(s)

Oscar Garcia-Cabrejo [e-mail]

References

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

See Also

Other hantush_jacob functions: hantush_jacob_WF_LT_dlogt, hantush_jacob_WF_LT, hantush_jacob_calculate_parameters, hantush_jacob_solution_dlogt, hantush_jacob_solution_initial, hantush_jacob_solution

Examples

td <- logseq(-2, 4, 50)
par <- list( beta = 0.5)
res <- hantush_jacob_well_function(td, par)
print(res)

khaors/pumpingtest documentation built on Nov. 15, 2019, 8:10 p.m.