Download Radioactive Dating

Radioactive Dating
If you know the half-life of a given radionuclide, you can in principle
use the decay of that radionuclide as a clock to measure time
intervals.
The decay of very long-lived nuclides, for example, can be used to
measure the age of rocks—that is, the time that has elapsed since
they were formed.
Such measurements for rocks from Earth and the Moon, and for
meteorites, yield a consistent maximum age of about 4.5 × 109 y.
The radionuclide 40K, for example, decays to 40Ar, a stable isotope of
the noble gas argon. The half-life for this decay is 1.25 × 109 y.
A measurement of the ratio of 40K to 40Ar, as found in the rock in
question, can be used to calculate the age of that rock.
Radioactive dating of a moon rock
In a Moon rock sample, the ratio of the number of (stable) 40Ar
atoms present to the number of (radioactive) 40K atoms is 10.3.
Assume that all the argon atoms were produced by the decay
of potassium atoms, with a half-life of 1.25 × 109 y. How old is
the rock?
Radiocarbon Dating
https://www.youtube.com/watch?v=Kcuz1JiMk9k
For measuring shorter time intervals, in the range of historical interest, radiocarbon
dating has proved invaluable.
The radionuclide 14C (with T1/2 = 5730 y) is produced at a constant rate in the upper
atmosphere as atmospheric nitrogen is bombarded by cosmic rays.
This radiocarbon mixes with the carbon that is normally present in the atmosphere (as
CO2) so that there is about one atom of 14C for every 1013 atoms of ordinary stable 12C.
Through biological activity such as photosynthesis and breathing, the atoms of
atmospheric carbon trade places randomly, one atom at a time, with the atoms of carbon
in every living thing, including broccoli, mushrooms, penguins, and humans.
Eventually an exchange equilibrium is reached at which the carbon atoms of every living
thing contain a fixed small fraction of the radioactive nuclide 14C.
This equilibrium persists as long as the organism is alive.
When the organism dies, the exchange with the atmosphere stops and the amount
of radiocarbon trapped in the organism, since it is no longer being replenished,
dwindles away with a half-life of 5730 y.
By measuring the amount of radiocarbon per gram of organic matter, it is possible
to measure the time that has elapsed since the organism died.
A 5.00 g charcoal sample from an ancient fire pit has a 14C activity of 63.0
disintegrations/min. A living tree has a 14C activity of 15.3 disintegrations/min per 1.00 g.
The half-life of 14C is 5730 y How old is the charcoal sample?