Sat {SoilHyP} | R Documentation |
Capillary saturation function
Description
Capillary saturation function of van Genuchten (unimodal or bimodal pore space distributions) and Brooks and Corey (unimodal pore space distribution).
Usage
Sat(suc, par.shp, modality = c("uni"), FUN.shp = "vg", suc.negativ = TRUE)
Arguments
suc |
Suction/pressure heads. Negative if suc.negativ = TRUE |
par.shp |
named parameter in list or vector |
modality |
pore size distribution ('uni' or 'bi') |
FUN.shp |
Funktion for soil hydraulic properties (vG or bc) (see details) |
suc.negativ |
set TRUE if suction/pressure heads are negative and FALSE if positive |
Details
- FUN.shp:
-
vG: van Genuchten (uni or bimodal) (vGM is working aswell)
bc: Brooks and Corey (uni)
- par.shp (van Genuchten):
-
alfa [1/L]: van Genuchten shape parameter
n [-]: van Genuchten shape parameter
m [-]: shape parameter (m = 1-(1/n) if missing) - par.shp (additional for bimodal (modality = 'bi')):
-
w2 [-]: weigthing between pore space distribution
alfa2 [1/L]: van Genuchten parameter alfa for second pore space distribution
n2 [-]: van Genuchten parameter n for second pore space distribution
- par.shp (Brooks and Corey):
-
alfa [1/L]: inverse of the air-entry value or bubbling pressure
lambda [-]: pore size distribution index
References
Van Genuchten, M. T. (1980). A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil science society of America journal, 44(5), 892-898.
Durner, W. (1994). Hydraulic conductivity estimation for soils with heterogeneous pore structure. Water Resources Research, 30(2), 211-223.
Brooks, R.H., and A.T. Corey (1964): Hydraulic properties of porous media. Hydrol. Paper 3. Colorado State Univ., Fort Collins, CO, USA.