Charcoal samples from Stonehenge in England were burned in \(\mathrm{O}_{2},\)
and the resultant \(\mathrm{CO}_{2}\) gas bubbled into a solution of
\(\mathrm{Ca}(\mathrm{OH})_{2}\) (limewater), resulting in the precipitation of
\(\mathrm{CaCO}_{3} .\) The \(\mathrm{CaCO}_{3}\) was removed by filtration and
dried. A \(788-\mathrm{mg}\) sample of the \(\mathrm{CaCO}_{3}\) had a
radioactivity of \(1.5 \times 10^{-2} \mathrm{~Bq}\) due to carbon-14. By
comparison, living organisms undergo 15.3 disintegrations per minute per gram
of carbon. Using the half-life of carbon- \(14,5715 \mathrm{yr},\) calculate the
age of the charcoal sample.