Description Usage Arguments Value Author(s) References See Also Examples
View source: R/theis_utilities.R
Function to calculate the theis well function for values of u < 1
1 |
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 |
This function returns the value of the dimensionless 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_solution
,
theis_well_function_large
,
theis_well_function
1 2 3 | u <- seq(0.01, 1, 0.01)
Ws <- theis_well_function_small(u)
plot(1/u, Ws, type = "l", log = "xy")
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