theis_well_function: theis_well_function

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

View source: R/theis_utilities.R

Description

Function to evaluate the Theis well function:

W(u) = \int_{u}^{∞} \frac{\exp{-u}}{u} du

Usage

1

Arguments

td

Dimensionless time t_n defined as

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

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

par

additional parameters

Value

This function returns the value of the Theis well function

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_large, theis_well_function_small

Examples

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u <- seq(0.05,30,0.05)
td <- 1.0/u
W <- theis_well_function(td, par)
plot(td, W, type = "l", log = "xy")

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