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 -mg sample of the \(\mathrm{CaCO}_{3}\) had a radioactivity of $1.5
\times 10^{-2}$ 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, 5700 yr, calculate the age of the charcoal sample.