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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. For c14_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. Use c14_decay_cambridge for the Cambridge constant, or a single numeric for other values.

Value

Vector the same length as x.

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 .

Examples

c14_age(0.9239)
#> [1] 0.999885
c14_f14c(636)
#> [1] -51854.61