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 (\(F^{14}C\) or \(pM\)) of a radiocarbon age.
Usage
c14_age(x, decay = c14::c14_decay_libby)
c14_f14c(x, decay = c14::c14_decay_libby)
Arguments
- x
For
c14_age()
, a vector of fraction modern (\(F^{14}C\)) measurements. Forc14_f14c()
, a vector of conventional radiocarbon ages.- decay
Decay constant. The default is the Libby constant (
c14_decay_libby
), which is the standard for calculating conventional radiocarbon ages. Usec14_decay_cambridge
for the Cambridge constant, or a single numeric for other values.
Details
c14_age()
calculates the conventional radiocarbon age, \(t\),
as defined by Stuiver and Polach (1977)
:
\[t = -\frac{1}{\lambda}\ln{F^{14}C}\]
c14_f14c()
implements the inverse of this function:
\[F^{14}C = e^{-\lambda t}\]
The decay constant conventionally used for calculating radiocarbon ages is the Libby decay constant, \(\lambda_L=8033^{-1}\). An alternative is the Cambridge decay constant, \(\lambda_C=8267^{-1}\) (Stenström et al. 2011) .
Reported radiocarbon ages are usually rounded based on the magnitude of the error (Stuiver and Polach 1977) . 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 (Bronk Ramsey 2008) .
References
Bronk Ramsey C (2008).
“Radiocarbon dating: revolutions in understanding.”
Archaeometry, 50(2), 249--275.
ISSN 0003-813X, 1475-4754, doi:10.1111/j.1475-4754.2008.00394.x
.
Stenström KE, Skog G, Georgiadou E, Genberg J, Johansson A (2011).
“A guide to radiocarbon units and calculations.”
Technical Report LUNFD6(NFFR-3111)/1-17/(2011), Lund University, Nuclear Physics.
Stuiver M, Polach HA (1977).
“Reporting of 14C Data.”
Radiocarbon, 19(3), 355--363.
ISSN 0033-8222, 1945-5755, doi:10.1017/S0033822200003672
.