step_aquifer_patch | R Documentation |
barker_herbert 1982 solution for radial patches.
step_aquifer_patch(
.rec,
time,
flow_rate = 0.01,
thickness = 1,
radius = 200,
radius_patch = 100,
specific_storage_inner = 1e-06,
specific_storage_outer = 1e-05,
hydraulic_conductivity_inner = 1e-04,
hydraulic_conductivity_outer = 1e-06,
n_stehfest = 12L,
role = "predictor",
...
)
.rec |
the R6 recipe object. |
time |
the time for evaluation (t) |
flow_rate |
the flow rate from the well (L^3/t) |
thickness |
the aquifer thickness (L) |
radius |
the distance to the observation well (L) |
role |
character - the name of the role |
... |
additional arguments |
The drawdown using the Theis model
Barker, J.A., and R. Herbert, 1982: Pumping tests in patchy aquifers, Ground Water, vol. 20, No. 2, pp. 150-155.
Butler, J.J., 1988: Pumping tests in nonuniform aquifers – The radially symmetric case, Journal of Hydrology, Vol. 101, pp. 15-30.
Other aquifer:
step_aquifer_constant_drawdown()
,
step_aquifer_grf()
,
step_aquifer_leaky()
,
step_aquifer_theis()
,
step_aquifer_theis_aniso()
,
step_aquifer_wellbore_storage()
dat <- data.frame(time = as.numeric(1:100))
formula <- as.formula(time~.)
frec = recipe(formula = formula, data = dat) |>
step_aquifer_patch(time = time, flow_rate = 0.01) |>
plate()
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