Description Usage Arguments Details Value Author(s) References Examples
Visulisation of the Soil Water Retention Curve van Genuchten Model (1980). For soil water calculation from soil water pressure head (hPa or cm water column) the package soilwater is used. Density functions for provided soil depths are visualized as side plots.
1 2 | Geotop_VisSoilWaterRet_gg(alpha, n, theta_sat, theta_res, accurate=10,
observed=NULL, add_ref_curves=TRUE)
|
alpha |
alpha van Genuchten parameter [1/m]; inverse of a length - scale parameter |
n |
N van Genuchten parameter [-]; shape parameter |
theta_sat |
saturated soil water content [m³/m³] |
theta_res |
residual soil water content [m³/m³] |
accurate |
default = 10: water potential is given as seq(1,10^7,10), for accurate plotting set argument 1 |
observed |
numeric data.frame, providing observed soil moisture data [m³/m³] (first column, named SWC) and water potential [hPa] (second column, named SWP) and soil depth [cm] (third coumn, named depth) |
add_ref_curves |
boolean, default = TRUE: reference soil water retention curves are added for clay, loam and sand; van Genuchten parameterisation according to ROSETTA manual |
colors |
colors for water retention curves and density functions, default = NULL: grey color range is used |
If multiple vanGenuchten models should be visualised, simply provide alpha, n, theta_sat, and theta_res values as vectors.
gg table object
Johannes Brenner, Johannes.Brenner@eurac.edu
Van Genuchten, M. (1980). A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal, 44, 892–898.
1 2 3 4 5 6 7 8 9 10 11 12 13 14 | ## Not run:
library(AnalyseGeotop)
data("Kaltern_SoilWatRet")
colors <- c("red","#E69F00","blue","darkgreen")
gg <- Geotop_VisSoilWaterRet_gg(alpha = parameter$alpha, n = parameter$n,
theta_sat = parameter$thetaS,
theta_res = rep(.05,length(parameter$alpha)),
accurate = 10,
add_ref_curves = T, observed = observed,
colors = colors)
## End(**Not run**)
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