View source: R/boulton_utilities.R
boulton_solution_initial | R Documentation |
Function to calculate the initial values of the hydraulic parameters of the Boulton model
boulton_solution_initial(ptest)
ptest |
A pumping_test object |
A list with:
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
\phi = \frac{\alpha_{1} r^{2} S}{T}
where \alpha_{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.
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
data(boulton)
ptest <- pumping_test("Well1", Q = 0.03, r = 20, t = boulton$t, s = boulton$s)
boulton.sol <- boulton_solution_initial(ptest)
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