d18O_H2O {isogeochem} | R Documentation |
Water d18O value
Description
d18O_H2O()
calculates the d18O value of the ambient water
from the d18O value of a carbonate and its growth temperature.
Usage
d18O_H2O(temp, d18O_c_VSMOW, min, eq)
Arguments
temp |
Carbonate growth temperature (°C). |
d18O_c_VSMOW |
Carbonate d18O value expressed on the VSMOW scale (‰). |
min |
Mineralogy. Options are |
eq |
Equation used to calculate the equilibrium 18O/16O oxygen isotope
fractionation factor between carbonate and water.
Options depend on mineralogy and listed in |
Value
Returns the water d18O value expressed on the VSMOW scale (‰).
Note
Use to_VSMOW()
and to_VPDB()
to convert between
the VSMOW and VPDB scales.
References
References are listed in the description of a18_c_H2O()
.
See Also
d18O_c()
calculates the equilibrium d18O value of a carbonate
grown at a given temperature.
temp_d18O()
calculates growth temperatures from oxygen isotope data.
Examples
d18O_H2O(temp = 33.7, d18O_c_VSMOW = 14.58,
min = "calcite", eq = "Coplen07")
d18O_H2O(temp = 25, d18O_c_VSMOW = to_VSMOW(-7.47),
min = "aragonite", eq = "GK86")