Description Usage Arguments Value Methods Examples
View source: R/anem_potentials.R
Estimate the radius of influence of a well
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... |
Variable parameters, depending on the method used. Single numbers or vectors (of equal length) |
method |
String containing the name of the desired method |
A numeric value indicating the horizontal radius of influence of the well.
The methods below are taken from Fileccia (2015). Acque
Sotterranee - Italian Journal of Groundwater
(http://www.doi.org/10.7343/AS-117-15-0144).
The following strings can be input for the method
variable, and must be accompanied
by the corresponding variables as part of the ...
input:
R=√{2.25 Tr t / S}, for confined aquifer after short pumping period. (Cooper and Jacob, 1946)
R=√{1.9 Ksat h t / n}, for unconfined aquifers (Aravin and Numerov, 1953)
R=3000 s √{Ksat}, Sichardt formula for unconfined aquifers (Cashman and Preene, 2001)
Where:
R = radius of influence [m]
Tr = transmissivity [m^2/s]
t = time [s]
S = storage
h = height of the water table above substratum [m]
n = effective porosity
Ksat = saturated hydraulic conductivity [m/s]
s = drawdown in the borehole [m]
These inputs can be single numbers or vectors of equal length.
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