d17O_c() now allows to choose from two different
17O/18O fractionation factors.NEWS.mda18_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)
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