Description Usage Arguments Value References
View source: R/d18O_evap_functions.R
Calculates the kinetic fractionation factor based on equation 6 in Krabeenhoft et al. (1990).
1 | d18O_evap_kinetic_frac(h, K = 14.3)
|
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. |
delta_epsilon - the kinetic fractionation factor (-)
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
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