gcsescience.com 21 gcsescience.com
Carbon Dating?
What is Carbon Dating?
The age of archaeological specimens can be
calculated
by looking at the amount of carbon-14 in a
sample.
The method is a form of radiodating called carbon dating.
Radiodating can also be used to date rocks.
How is Carbon-14
formed?
The isotope
carbon-14 is created at a constant rate in the upper
atmosphere by cosmic rays acting on nitrogen. The carbon-14 which
is formed is radioactive and decays to produce nitrogen
again.
There is therefore a fixed amount of
carbon-14
in the environment
which is a balance between the
rate at which it is formed in
the atmosphere and the rate at which it decays back to nitrogen.
How does Carbon
Dating work?
All living things take in carbon from the environment.
Plants take in carbon during photosynthesis.
Animals take in carbon when
they eat food because food
contains carbon.
All living
things therefore have carbon-14 in
them
at the same amount which is
present in the environment.
This amount is small. Only one in 850
billion carbon atoms
are the isotope
carbon-14. The others are
not radioactive.
They are carbon-12 (about 99%) and carbon-13 (about 1%).
When a living thing dies, it
stops taking in carbon from its
environment.
The amount of carbon-14 in it will
start to decrease
as the carbon-14 slowly
decays. The further back in time that
something died, the less
carbon-14
will be present in it today.
The half-life of
carbon-14 is
5,730 years.
Measuring the amount of carbon-14 in a sample
today can tell
you
how
long ago the thing
died and therefore the age
of the sample.
Carbon dating is very useful but also has its limitations.
Links Radioactivity Half-life Revision Questions
gcsescience.com Physics Quiz Index Radioactivity Quiz gcsescience.com
Home GCSE Chemistry GCSE Physics
Copyright © 2015 gcsescience.com. All Rights Reserved.