unitResponse {soilwater} | R Documentation |
The water table recharge: the response unit
Description
The water table recharge: the response unit
Usage
unitResponse(t, d = 1, D = 1, H = d, m = 100)
Arguments
t |
time coordinate |
d |
depth of unsaturated zone along the slope-normal direction |
D |
soil water diffusivity |
H |
soil depth |
m |
maximum limit of summary truncation. Default is 100. |
Note
This function calcletes the water-table recharge rate in a hillslope assuming:
1. Richards' Equation is linearized and reduced to the form of heat equation;
2. The diffusion water-table rate is connectedwith soil pressure head according with eq. 13 (Cordano and Rigon, 2008);
References
Cordano, E., and R. Rigon (2008), A perturbative view on the subsurface water pressure response at hillslope scale, Water Resour. Res., 44, W05407, doi:10.1029/2006WR005740. http://onlinelibrary.wiley.com/doi/10.1029/2006WR005740/pdf
Examples
library(soilwater)
t <- seq(0,2,by=0.001)
d <- c(1,0.75,0.5,0.25)
val1 <- unitResponse(t, d = d[1], D = 1, H = 1, m = 500)
val2 <- unitResponse(t, d = d[2], D = 1, H = 1, m = 500)
val3 <- unitResponse(t, d = d[3], D = 1, H = 1, m = 500)
val4 <- unitResponse(t, d = d[4], D = 1, H = 1, m = 500)
[Package soilwater version 1.0.5 Index]