theis_well_function_large: theis_well_function_large

Description Usage Arguments Value Author(s) References See Also Examples

View source: R/theis_utilities.R

Description

Function to calculate the theis well function for values of u > 1

Usage

1

Arguments

u

Dimensionless u variable defined as:

u=\frac{r^{2}S}{4Tt}

where r is the distance between the pumping and observation well in m, S is the storage coefficient (dimensionless), T is the Transmisivity in m2/s and t is the time in s

Value

This function returns the value of the dimensionless drawdown

Author(s)

Oscar Garcia-Cabrejo khaors@gmail.com

References

Theis, C. The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using groundwater storage. Transactions of the American Geophysical Union, 1935, 2, 519-524

See Also

Other theis functions: exponential_integral, theis_WF_LT_dlogt, theis_WF_LT, theis_calculate_parameters, theis_solution_dlogt, theis_solution_initial, theis_solution, theis_well_function_small, theis_well_function

Examples

1
2
u <- seq(1.0, 20.0, 0.5)
res <- theis_well_function_large(u)

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