c14_units | R Documentation |
Functions for calculating basic units used in radiocarbon measurements.
c14_age()
calculates the conventional radiocarbon age (CRA) from a fraction
modern measurement.
c14_f14c()
reverse-calculates the fractionation-corrected fraction modern
value (\mjeqnF^14CF14C or \mjeqnpMpM) of a radiocarbon age.
c14_age(x, decay = c14::c14_decay_libby)
c14_f14c(x, decay = c14::c14_decay_libby)
x |
For |
decay |
Decay constant. The default is the Libby
constant ( |
c14_age()
calculates the conventional radiocarbon age, \mjeqntt,
as defined by \insertCiteStuiver1977;textualc14:
t = -\frac1\lambda\lnF^14Ct = -1/l * ln(F^14C)
c14_f14c()
implements the inverse of this function:
F^14C = e^-\lambda tF14C = e^(-lt)
The decay constant conventionally used for calculating radiocarbon ages is the Libby decay constant, \mjeqn\lambda_L=8033^-1lL = 1/8033. An alternative is the Cambridge decay constant, \mjeqn\lambda_C=8267^-1lC = 1/8267 \insertCiteStenstrom2011c14.
Reported radiocarbon ages are usually rounded based on the magnitude of the error \insertCiteStuiver1977c14. For this reason, reverse-calculating fraction modern from a radiocarbon age is unlikely to return the precise original measurement of the sample.
Where available, fraction modern is the recommended measurement for calibration \insertCiteBronk_Ramsey2008c14.
Vector the same length as x
.
c14_age(0.9239)
c14_f14c(636)
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