c14_units: Radiocarbon unit calculations

c14_unitsR Documentation

Radiocarbon unit calculations

Description

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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 (\mjeqnF^14CF14C or \mjeqnpMpM) 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 (\mjeqnF^14CF14C) 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.

Details

c14_age() calculates the conventional radiocarbon age, \mjeqntt, as defined by \insertCiteStuiver1977;textualc14:

\mjdeqn

t = -\frac1\lambda\lnF^14Ct = -1/l * ln(F^14C)

c14_f14c() implements the inverse of this function:

\mjdeqn

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.

Value

Vector the same length as x.

References

\insertAllCited

Examples

c14_age(0.9239)
c14_f14c(636)

joeroe/c14 documentation built on Nov. 24, 2024, 11:47 p.m.