Isotope
Atoms with the same atomic number but a different mass number
Radioactive Decay
Unstable isotopes decay into other elements and spit out radiation as they try to become more stable
Radioactive Decay Spits Out
Apha Beta Gamma Neutrons
Ionising Radiation
Knocks electrons off atoms Creating positive ions
Ionising Power
How easily they can do this
Alpha Particles
Helium Nuclei
Alpha Radiation
When an alpha particle is emitted from a nucleus Two protons and two neutrons
Penetration of Alpha
Not very as they can only travel a few cm in the air and are absorbed by a piece of paper
Ionising of Alpha
Strongly Ionising
Beta Particles
High speed electrons emitted from a nucleus No mass Charge of -1
Penetration of Beta
Moderately Far
Beta Ionising
Moderately Ionising
Beta Range in Air
Few metres Absorbed by a sheet of aluminium
Gamma Rays
Electromagnetic waves with a short wavelength released by the nucleus
Gamma Penetration
Far into materials Absorbed by thick lead or metres of concrete
Gamma Ionising
Weakly ionising tends to pass through materials rather than collide with atoms
Nuclear Equations
Show radioactive decay using elemental symbols Atom Before Decay --> Atom After Decay
Golden Rule of Nuclear Equations
Total Mass and Atomic Numbers must be equal on both sides
Alpha Decay
Made up of two protons and two neutrons When an atom emits an alpha particle, its atomic number reduces by two and its mass number by four Charge decreases
Beta Decay
Neutron is turned into a proton and a fast-moving electron is released Increase in positive charge and therefore the atomic number 0-1e
Gamma Decay
Ways of getting rid of excess energy No change in mass or atomic number
Half Life
Time taken for the number of radioactive nuclei in an isotope to half
Why can you not predict when a nuclei will emit radiation
Because radioactive decay is a totally random process
Why do we use Half Life?
Makes predictions about radioactive sources
Activity
The rate at which a source decays Bq (1Bq is 1 decay per second)