fitbusscher {soilphysics} | R Documentation |
Self-starting Nls Busscher's (1990) Model for Soil Penetration Resistance
Description
Function to self start the nonlinear Busscher's (1990) model for penetration
resistance, i.e., Pr = b0 * (\theta ^ {b1}) * (Bd ^ {b2})
. It creates initial
estimates (by log-linearization) of the parameters b0, b1 and b2 and uses them
to provide its least-squares estimates through nls
.
Usage
fitbusscher(Pr, theta, Bd, ...)
Arguments
Pr |
a numeric vector containing penetration resistance values. |
theta |
a numeric vector containing soil moisture values at which to evaluate the model. |
Bd |
a numeric vector containing bulk density values at which to evaluate the model. |
... |
further arguments to |
Value
A nls
output (see help(nls)
).
Author(s)
Anderson Rodrigo da Silva <anderson.agro@hotmail.com>
References
Busscher, W. J. (1990). Adjustment of flat-tipped penetrometer resistance data to common water content. Transactions of the ASAE, 3:519-524.
See Also
fitlbc
, nls
, summary.nls
,
predict.nls
, Rsq
Examples
data(compaction)
attach(compaction)
out <- fitbusscher(Pr = PR, theta = Mois, Bd = BD)
summary(out)
Rsq(out)
# 3D plot
X <- seq(min(Mois), max(Mois), len = 30) # theta
Y <- seq(min(BD), max(BD), len = 30) # Bd
f <- function(x, y) coef(out)[1] * (x^coef(out)[2]) * (y^coef(out)[3])
Z <- outer(X, Y, f)
persp(X, Y, Z,
xlab = "Soil moisture",
ylab = "Soil bulk density",
zlab = "Penetration resistance",
ticktype = "detailed",
phi = 20, theta = 30)
# End (not run)