Description Usage Arguments Details Value Author(s) See Also Examples
View source: R/alpha_constants.R
This function accesses the appropriate method to calculate the
α-dependent constant associated with the choice of c.type
.
There are currently four such constants, which correspond to
Equations 10, 11, 18, 19 in Kitagawa et al (2011).
This function is not likely to be needed by the user.
1 2 3 4 | alpha_constants(alpha = 0, c.type = c("Phi", "Psi", "A", "Kel"))
## Default S3 method:
alpha_constants(alpha = 0, c.type = c("Phi", "Psi", "A", "Kel"))
|
alpha |
the constant alpha (see |
c.type |
the constant to calculate |
"alpha"
?The constant α is a function of frequency ω as well as aquifer and well parameters; it is formally defined as
α \equiv R_S √{ω S / T}
where S is the storativity, T is the aquifer's effective transmissivity, and R_S is the radius of the screened portion of the well.
The various constants which may be calculated with this function are
Phi
Given as Φ in Eqn. 10
Psi
Given as Ψ in Eqn. 11
A
Given as A_i, i=1,2 in Eqns. 18, 19
Kel
The complex Kelvin functions (see Abramowitz and Stegun, 1972)
Complex matrix having values representing the constant
represented by c.type
,
as well as any other α-dependent constants
which are needed in the computation.
A. J. Barbour <andy.barbour@gmail.com>
omega_constants
, well_response
Other ConstantsCalculators:
kitagawa-constants
,
omega_constants()
1 2 3 | alpha_constants() # kelvin::Keir gives warning
alpha_constants(1) # defaults to constant 'Phi' (note output also has Kel)
alpha_constants(1:10, c.type="A") # constant 'A' (again, note output)
|
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