A living specimen in equilibrium with the atmosphere contains one atom of 14C (half-life = 5730 yr) for every 7.7 ✕ 1011 stable carbon atoms. An archeological sample of wood (cellulose, C12H22O11) contains 20.6 mg of carbon. When the sample is placed inside a shielded beta counter with 88.0% counting efficiency, 765 counts are accumulated in one week. Assuming that the cosmic-ray flux and the Earth's atmosphere have not changed appreciably since the sample was formed, find the age of the sample.
Total number of carbon atoms in given sample
N = 20.6e-3 g * 6.02e23 molecules / mol / 12 g/mol
N = 1.033e21 atoms
one in these atoms is C-14 so,
Number of C-14
N' = 1.033e21 / 7.7e11
N' = 1.342e9
Now, we find decay constant
= ln 2 / T1/2
= ln 2 / 5730
= 3.83e-12 / sec
Initial activity
R = 3.83e-12 * 1.342e9 * 7 * 86400
R = 3108.587 decays / week
at some given time
R' = 765 / 0.88 = 869.32 decays / week
Now, from decay equation
ln ( R' / R ) = - t
so,
t = -1/ * ln ( R' / R)
t = -1/ 3.83e-12 * ln ( 869.32 / 3108.587)
t = 3.326e11 seconds
or
t = 1.053e4 years
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