step_aquifer_wellbore_storage | R Documentation |
Papadopulos-Cooper 1967 solution for wellbore storage.
step_aquifer_wellbore_storage(
.rec,
time,
flow_rate = 1,
radius = 0.15,
radius_casing = 0.15,
radius_well = 0.15,
thickness = 1,
specific_storage = 1e-06,
hydraulic_conductivity = 1e-04,
n_terms = 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) |
radius |
distance from center of well |
radius_casing |
radius of casing in the interval over which the water level declines |
radius_well |
effective radius of well screen or open hole |
thickness |
the aquifer thickness (L) |
specific_storage |
specific storage of aquifer (L/L) |
hydraulic_conductivity |
the hydraulic conductivity (L/t) |
role |
character - the name of the role |
... |
additional arguments |
The drawdown using the Papadopulos-Cooper model
Papadopulos, I.S. and H.H. Cooper, 1967. Drawdown in a well of large diameter, Water Resources Research, vol. 3, no. 1, pp. 241-244.
Other aquifer:
step_aquifer_constant_drawdown()
,
step_aquifer_grf()
,
step_aquifer_leaky()
,
step_aquifer_patch()
,
step_aquifer_theis()
,
step_aquifer_theis_aniso()
dat <- data.frame(x = 10^seq(-5, 2, length.out = 100),
y = rep(0.01, 100))
formula <- as.formula(y~x)
frec = recipe(formula = formula, data = dat) |>
step_aquifer_wellbore_storage(time = x,
flow_rate = 10.0,
hydraulic_conductivity = 10.0,
specific_storage = 1e-4) |>
prep() |>
bake()
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