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Radiation Hazards and Safety is taught in the note for Radioactivity. Read it below and look for the section on this topic.

Radioactivity

15 min read

The nucleus of an atom

An atom has a tiny, dense nucleus of protons and neutrons (together called nucleons), surrounded by electrons. The atomic (proton) number Z is the number of protons. The mass (nucleon) number A is the number of protons plus neutrons. Isotopes are atoms of the same element (same Z) with different numbers of neutrons, such as carbon-12 and carbon-14.

Notation: ¹⁴₆C has 6 protons and 14 − 6 = 8 neutrons.

Natural radioactivity

Some nuclei are unstable and give out radiation to become more stable. This is radioactive decay. It is random (we cannot say when a particular nucleus will decay) and spontaneous (it is not affected by temperature, pressure or chemical reactions). There are three kinds of radiation.

Alpha (α)Beta (β)Gamma (γ)
NatureHelium nucleus (2 protons + 2 neutrons)A fast electron from the nucleusElectromagnetic wave of very short wavelength
Charge+2−10
PenetrationStopped by paper or a few centimetres of airStopped by a few millimetres of aluminiumReduced by thick lead or concrete
Ionising powerStrongestMediumWeakest
Deflected by magnetic field?Yes (slightly)Yes (strongly, opposite way)No
Effect on the nucleusA decreases by 4, Z by 2A unchanged, Z increases by 1No change in A or Z
Penetration of radiationA radioactive source on the left. Alpha particles are stopped by a sheet of paper. Beta particles pass through paper but are stopped by a few millimetres of aluminium. Gamma rays pass through both and are only reduced by thick lead or concrete.sourceαpaperβaluminiumγthick lead
DecayEquation example
Alpha²³⁸₉₂U → ²³⁴₉₀Th + ⁴₂He
Beta¹⁴₆C → ¹⁴₇N + ⁰₋₁e
GammaFollows α or β decay when the nucleus is left excited

Half-life

Half-life
The time taken for half of the radioactive nuclei in a sample to decay. It is constant for a given isotope.
Radioactive decay and half-lifeA graph of the number of undecayed nuclei against time. It falls by a half in each equal time interval called the half-life. After one half-life half of the nuclei remain, after two a quarter, after three an eighth.timeundecayed nuclei1 half-life23½¼N₀
N₀ is the starting number of nuclei (or the starting activity or mass), t is the time and T is the half-life.
Try itRadioactive decay

Choose the half-life and the time that has passed. Find the fraction and percentage of the sample left.

The activity halves every 5 days: 100, 50, 25, 12.5 …
Worked exampleHalf-life calculation

A sample of a radioactive isotope has a half-life of 6 hours. What fraction is left after 24 hours?

  1. 24 hours is 4 half-lives.
  2. Each half-life halves the amount.

Answer: One-sixteenth (6.25%) is left.

Artificial radioactivity and uses

Stable nuclei can be made radioactive by bombarding them with neutrons in a nuclear reactor or with particles from an accelerator. These radioisotopes have many uses.

UseRadioisotope and idea
Medical tracersIodine-131 to study the thyroid; technetium-99m for scans
Treating cancerCobalt-60 gamma rays destroy cancer cells (radiotherapy)
Sterilising instruments and foodGamma rays kill germs
Thickness gaugesBeta particles passing through paper or plastic; fewer pass through if the sheet is thicker
Smoke alarmsAmericium-241 alpha source; smoke reduces the ionisation current
DatingCarbon-14 half-life 5 730 years dates once-living objects; uranium dates rocks
Leak tracingA tracer in a pipe is detected where it leaks out

Radiation hazards and safety

Radiation ionises atoms and can damage cells, causing burns, cancer and genetic damage. Everybody receives a little background radiation from rocks, radon gas, cosmic rays and food. Safety rules: use the smallest dose, keep the longest distance, and spend the shortest time; shield with lead; handle sources with tongs, never by hand; store in lead containers; wear a film badge to measure the dose.

Nuclear fission and fusion

Nuclear fission and a chain reactionA slow neutron strikes a uranium-235 nucleus, which splits into two smaller nuclei such as barium and krypton, releasing a lot of energy and two or three more neutrons. Each of these neutrons can split another nucleus, so a chain reaction grows unless it is controlled.U-235BaKr+ energy…
FissionFusion
What happensA heavy nucleus (uranium-235) splits into two smaller nuclei and more neutronsTwo light nuclei (hydrogen isotopes) join to make helium
EnergyLarge energy per atomEven more energy per kilogram
ConditionsSlow neutrons; chain reaction controlled in a reactor by boron or cadmium rodsMillions of degrees (in the Sun)
UseNuclear power stations, atomic bombsThe Sun and stars; research reactors
WasteLong-lived radioactive wasteLittle long-lived waste
Einstein: a small loss of mass (the mass defect) in a nuclear reaction is changed into a very large amount of energy. c = 3 × 10⁸ m/s.
Check yourself Which radiation is the most penetrating?
Check yourself After an alpha decay the mass number of the nucleus…
Check yourself A radioisotope has a half-life of 10 days. How much of 80 g is left after 30 days?

Key terms

Isotopes
Atoms with the same number of protons but different numbers of neutrons.
Half-life
The time for half of the radioactive nuclei in a sample to decay.
Fission
The splitting of a heavy nucleus into two lighter nuclei.
Fusion
The joining of two light nuclei into one heavier nucleus.

Summary

  • Radioactive decay is random and spontaneous; α, β and γ differ in nature, penetration and ionisation.
  • Half-life: N = N₀ (½)^(t/T).
  • Radioisotopes are used in medicine, industry and dating; radiation is hazardous and needs shielding.
  • Fission splits heavy nuclei; fusion joins light nuclei; E = mc².