Nothing
d17O_c()
now allows to choose from two different 17O/18O fractionation factors.NEWS.md
a18_c_H2O()
Can now calculate the dolomite/water 18O/16O fractionation factor.a18_CO2acid_c()
Can now calculate the dolomite/CO2 18O/16O AFF.a18...()
functions now return meaningful errors.d17O_c()
Can now take into account a non-zero D17O value for the ambient water.mix_d17O()
was overhauled. It now allows D17O values as input and specifying the resolution of the output. The output of the function now returns the d17O values as the fourth element in the data frame.d17O_qz()
to calculate equilibrium oxygen isotope values for quartz.meteoric_waters
is a compilation of d17O and d18O values for meteoric waters.D17O()
calculates triple oxygen isotope value from d18O and d17O valuesyork_plot()
returns silentlya18_CO2g_H2O()
a18_CO2aq_H2O()
a18_CO3_H2O()
a18_HCO3_H2O()
a13_CO2g_CO2aq()
X_absorption()
X_DIC()
temp_D48()
the curve_intersect() part was slimmed downtemp_D47()
and temp_D48()
both result in a similar data frame (length = 2) if errors are specifiedtemp_D47()
, temp_D48()
, and temp_d18O()
are optimize
-da18_c_H2O()
a18_c_H2O()
a18_H2O_OH()
: "Z21-X3LYP" —> "Z20-X3LYP"isogeochem
with vignettes now works (#2, @japhir)Any scripts or data that you put into this service are public.
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