shypFun.04110: Unimodal Brooks-Corey Model

In spsh: Estimation and Prediction of Parameters of Various Soil Hydraulic Property Models

Description

Calculates the soil hydraulic property function values based on given pressure heads \insertCiteKosugi.1996spsh.

Usage

shypFun.04110(p, h)

Arguments

p	vector of the 6 Brooks-Corey model parameters, order is sensitve and has to be given as: thr residual water water content [cm cm-3] ths saturated water water content [cm cm-3] alf air entry pressure head [cm^-1] bet effective model parameter [ - ] Ks saturated conductivity [cm d-1] tau exponent of Se in the capillary conductivity model, sometimes denoted in the literature as l [-]
h	pressure heads [cm] for which the corresponding retention and conductivity values are calculated.

Details

The function solves analytically the spec. water capacity function and integral to the capillary bundle model.

Value

returns a list with calculations at specified h:

theta	calculated volumetric moisture content
Se	calculated saturation
cap	returns NA; not supported
psd	returns NA; not supported
Kh	Hydraulic conductivity values

Note

The Muealm integral is solved numerically

References

\insertRef

Brooks.1964spsh

Examples

p      <- c(0.1, 0.4, .01, .3, 100, .5)
h      <- 10^seq(-2, 6.8, length = 197)
shyp.L <- shypFun.04110(p, h)

spsh documentation built on April 14, 2020, 6:37 p.m.