A radioactive substance contains unstable nuclei that
become stable by emitting radiation
Alpha, beta and gamma radiation
Radioactive decay cannot be predicted
The origins of background radiation are: air (radon), medical (x-rays),
the ground (rocks), food and drink, cosmic rays from space, nuclear
weapons, air travel and nuclear reactors
Rutherford used measurements from alpha scattering
experiments to prove that atoms have small + charged nuclei
where most of the mass is located
'Plum pudding model' couldn't explain why
some alpha particles were scattered
through large angles
The nuclear model of the atom explains
why alpha particles are scattered
Isotopes of an element are atoms with same number of
protons but different number of neutrons - same atomic
number but different mass number
A magnetic or electric field can separate a
beam of alpha, beta and gamma
They ionise substances they pass through,
ionisation can kill or damage cells
The half life of radioactive isotopes is the
average time taken for the number of nuclei in
a sample to halve
The activity of a radioactive source is
the number of nuclei that decay per sec
The use of a radioactive isotope depends on:
1) its half life
2) type of radiation given out
For monitoring, isotope needs a long half life
Tracers should be beta or gamma which last
long enough to monitor but not too long
For radio active dating of a sample an isotope with a similar half life
needs to be used