View source: R/alpha_constants.R
| alpha_constants | R Documentation |
\alphaThis function accesses the appropriate method to calculate the
\alpha-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.
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 \alpha is a function of frequency \omega as well
as aquifer and well parameters; it is formally defined as
\alpha \equiv R_S \sqrt{\omega 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
PhiGiven as \Phi in Eqn. 10
PsiGiven as \Psi in Eqn. 11
AGiven as A_i, i=1,2 in Eqns. 18, 19
KelThe complex Kelvin functions (see Abramowitz and Stegun, 1972)
Complex matrix having values representing the constant
represented by c.type,
as well as any other \alpha-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()
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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