d18O_evap_kinetic_frac: Kinetic Fractionation Factor

Description Usage Arguments Value References

View source: R/d18O_evap_functions.R

Description

Calculates the kinetic fractionation factor based on equation 6 in Krabeenhoft et al. (1990).

Usage

1

Arguments

h

relative humidity normalized to the temperature of the surface water (-)

K

constant determinded by wind tunnel experiments for different isotopes, defaults to K(18O) = 14.3.

Value

delta_epsilon - the kinetic fractionation factor (-)

References

Krabbenhoft, D. P., C. J. Bowser, M. P. Anderson, and J. W. Valley. (1990). Estimating Groundwater Exchange with Lakes: 1. The Stable Isotope Mass Balance Method. Water Resources Research, 26(10):2445-2453. https://doi.org/10.1029/WR026i010p02445


cvoter/isoH2Obudget documentation built on March 29, 2020, 11:07 a.m.