Radioactivity Flashcards
Alpha radiation
Each alpha particle is a helium nucleus - 2 protons and 2 neutrons. Charge = +2e
Alpha particles have a large mass and charge so they interact with surrounding particles. They are strongly ionising and have a very short range.
They are stopped by paper
Beta radiation
Consists of fast moving electrons or positrons
Have a smaller mass and charge so they are less ionising and have a shorter range in air. It takes 1-3mm of aluminium to stop them
Gamma radiation
High energy photons with wavelength <10^-13 m. They travel at the speed of light so carry no charge
Low ionisation and large range
Takes a few centimeters of lead to stop
Parent nucleus
Nucleus before decay
Daughter nucleus
New nucleus after decay
Random
We cannot predict when a particular nucleus will decay or which will decay next.
Each nucleus in a sample has the same chance of decaying per unit time
Spontaneous
Decay of nuclei is not affected by presence of other nuclei in the sample or other factors such as pressure
Half-life
The time it takes for half the number of active nuclei in the sample to decay
t1/2
Activity
The rate at which nuclei decay
1 Becquerel is 1 decay per second
Decay constant
Probability of decay of an individual nucleus per unit time
A = decay constant x N
Decay constant equation derrivation
ΔN ∝ NΔt
ΔN/Δt ∝ -N
A∝ -N
A=λN
Nuclei decay equation
N=N0e^−λt
Where N0 is the number of undecayed nuclei at t-0
λ = ln(2)/half life
A=A0e^−λt
Carbon dating
Uses the ratio of Carbon-14 to Carbon-12 to tell how long an organism has been dead, as Carbon-14 decays over time.
Ratio is constant in a living organism but no new carbon is taken in after death