hydraulicCutOff {soilphysics} | R Documentation |
The matric potential at the point of hydraulic cut-off obtained from DE (Dexter et al., 2008) and GG (Groenevelt & Grant, 2004) water retention curves.
Description
The pore water suction at the point of hydraulic cut-off occurs at the point where the residual water content, obtained from Dexter et al. (2008), intercepts with the Groenevelt & Grant (2004) retention curve.
Usage
hydraulicCutOff(theta_R, k0, k1, n, x0 = 6.653)
Arguments
theta_R |
a parameter that represents the residual water content at the the Dexter's (2008) Water Retention Model. |
k0 |
a parameter value, extracted from the water retention curve based on the Groenevelt & Grant (2004) formula. |
k1 |
a parameter value, extracted from the water retention curve based on the Groenevelt & Grant (2004) formula. |
n |
a parameter value, extracted from the water retention curve based on the Groenevelt & Grant (2004) formula. |
x0 |
the value of pF (pore water suction) at which the soil water content becomes zero. The default is 6.653. |
Value
The water suction at the point of hydraulic cut-off.
Author(s)
Anderson Rodrigo da Silva <anderson.agro@hotmail.com>
References
Dexter, A.R.; Czyz, E.A.; Richard, G.; Reszkowska, A. (2008). A user-friendly water retention function that takes account of the textural and structural pore spaces in soil. Geoderma, 143:243–253.
Groenevelt, P.H.; Grnat, C.D. (2004). A new model for the soil-water retention curve that solves the problem of residual water contents. European Journal of Soil Science, 55:479–485.
See Also
Examples
# Dexter et al. (2012), Table 4A
hydraulicCutOff(0.1130, 6.877, 0.6508, 1.0453)
hydraulicCutOff(0.1122, 12.048, 0.4338, 2.0658)
# End (not run)