r: Equation of capillary

In soilphysics: Soil Physical Analysis

Equation of capillary

Description

The equivalent pore radius as a function of soil water tension.

Usage

r(h, surface.tension.water=0.072, water.density=1000, water.pore.contact.angle=0)

Arguments

h	The water tension (hPa).
surface.tension.water	Surface tension of water (N/m).
water.density	Density of water (kg/m^3).
water.pore.contact.angle	Water pore contact angle (degrees).

Value

The equivalent pore radius, in micrometer..

Author(s)

Renato Paiva de Lima <[e-mail]>

References

Ghiberto, P. J., Imhoff, S., Libardi, P. L., Silva, A. P. D., Tormena, C. A., Pilatti, M. A. (2015). Soil physical quality of Mollisols quantified by a global index. Scientia Agricola, 72(2):167-174.

Examples

x <- seq(log10(1), log10(15000), len=50)
h <- 10^x
y <- r(h=h)
plot(x=h, y=y, log="yx", xlab="h (hPa)", yaxt='n', ylab="", ylim=c(0.1, 1500))
ax <- c(0.1, 1, 10, 100, 1000, 1500)
axis(2,at=ax, labels=ax)
mtext("Pore radius"~ (mu*m), 2, line=2.5)

# End (not run)

soilphysics documentation built on June 7, 2022, 5:06 p.m.