boulton_solution: boulton_solution

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

View source: R/boulton_utilities.R

Description

Function to calculate the drawdown of a Boulton model

Usage

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boulton_solution(ptest, a, t0, t1, phi, t)

Arguments

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

Value

A vector with the calculated drawdown

Author(s)

Oscar Garcia-Cabrejo khaors@gmail.com

References

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

See Also

Other boulton functions: boulton_WF_LT, boulton_calculate_parameters, boulton_solution_dlogt, boulton_well_function

Examples

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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)

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