Description Usage Arguments Value Author(s) References See Also Examples
View source: R/boulton_utilities.R
Function to calculate the drawdown of a Boulton model
1 | boulton_solution(ptest, a, t0, t1, phi, t)
|
ptest |
A pumping_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 (early time) |
t1 |
Intercept of the straight line fitted to the drawdown data using the Cooper-Jacob approach (late time) |
phi |
Delay parameter. Dimensionless parameter defined as φ = \frac{α_{1} r^{2} S}{T} where α_{1} is a fitting parameter without a physical estimation, r is the distance between the pumping and observation well, S is the storage coefficient and T is the transmissivity. |
t |
Numeric vector with the time values |
A vector with the calculated drawdown
Oscar Garcia-Cabrejo khaors@gmail.com
Boulton, N. The drawdown of the water-table under non-steady conditions near a pumped well in an unconfined formation. Proceedings of the Institution of Civil Engineers, 1954, 3, 564-579
Other boulton functions: boulton_WF_LT
,
boulton_calculate_parameters
,
boulton_solution_dlogt
,
boulton_well_function
1 2 3 4 5 | data(boulton)
ptest <- pumping_test("Well1", Q = 0.03, r = 20, t = boulton$t, s = boulton$s)
boulton_sol0 <- boulton_solution_initial(ptest)
boulton_sol1 <- boulton_solution(ptest, boulton_sol0$a, boulton_sol0$t0,
boulton_sol0$t1, boulton_sol0$phi, boulton$t)
|
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