Description Usage Arguments Value Author(s) References See Also Examples
View source: R/theis_utilities.R
Function to calculate the drawdown using the Theis solution
1 | theis_solution(ptest, a, t0, t)
|
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 |
A numeric vector with the drawdown
Oscar Garcia-Cabrejo khaors@gmail.com
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
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
1 2 3 4 5 6 7 8 | # 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)
|
Add the following code to your website.
For more information on customizing the embed code, read Embedding Snippets.