theis_solution: theis_solution

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

View source: R/theis_utilities.R

Description

Function to calculate the drawdown using the Theis solution

Usage

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theis_solution(ptest, a, t0, t)

Arguments

ptest

A pumpint test object

a

slope of the straight line fitted to the drawdown data using the Cooper-Jacob approach

t0

intercept of the straight line fitted to the drawdown data using the Cooper-Jacob approach

t

Numeric vector with the time values

Value

A numeric vector with the 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_well_function_large, theis_well_function_small, theis_well_function

Examples

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# Data from a confined aquifer
data(theis)
ptest <- pumping_test('Well1', Q = 1.3e-3, r = 200, t = theis$t, s = theis$s)
res <- theis_solution_initial(ptest)
s_model <- theis_solution(ptest,res$a, res$t0, theis$t)
#Compare drawdown from model with measurements
mse <- sqrt(mean((s_model-theis$s)^2))
print(mse)

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