Radioactivity
CAIE Physics IGCSE: Radioactivity Notes
Some isotopes are unstable due to an imbalance of protons and neutrons. They become stable by releasing energy in the form of radiation; this process is called radioactive decay.
5.2 Radioactivity
5.2.1 Detection of Radioactivity
Background radiation is low-level ionising radiation present in the environment from natural and man-made sources:
- Radon gas from rocks
- Radiation from food and drink (e.g., radioactive potassium in bananas)
- Cosmic rays from space
- Medical and industrial waste
It is detected using a Geiger-Muller (GM) tube connected to a counter.
- Count rate is the number of decays detected per second (measured in Becquerels, Bq) or per minute.
- The corrected count rate is found by subtracting the background count rate from the measured count rate:
Corrected Count Rate = Count Rate with Source - Background Count Rate
5.2.2 The Three Types of Nuclear Emission
Radiation is emitted spontaneously and randomly from the nuclei of unstable isotopes.
| Property | Alpha (α) Particle | Beta (β) Particle | Gamma (γ) Ray |
|---|---|---|---|
| Nature | Helium nucleus (2p + 2n) | High-speed electron | Electromagnetic wave |
| Symbol | 42α or 42He | 0-1β or 0-1e | 00γ |
| Charge | +2 | -1 | 0 |
| Mass | 4 | 1/1840 (negligible) | 0 |
| Ionising Power | Very High | Moderate | Very Low |
| Penetration | Low (stopped by paper/skin) | Moderate (stopped by few mm aluminium) | Very High (stopped by thick lead/concrete) |
| Deflection by Fields | Slightly by electric/magnetic fields | Greatly by electric/magnetic fields | Not deflected |
Rule of Thumb: The more ionising a radiation is, the less penetrating it is.
5.2.3 Radioactive Decay
Radioactive decay is the process by which an unstable nucleus becomes more stable by emitting radiation. It changes the composition of the nucleus.
1. Alpha (α) Decay:
- The nucleus emits an alpha particle (2 protons + 2 neutrons).
- Mass number decreases by 4, Atomic number decreases by 2.
- The atom changes to a different element.
- Equation:
AZX → A-4Z-2Y + 42α
2. Beta (β⁻) Decay:
- A neutron in the nucleus transforms into a proton and emits a beta particle (electron).
- Mass number stays the same, Atomic number increases by 1.
- The atom changes to a different element.
- Equation:
AZX → AZ+1Y + 0-1β
3. Gamma (γ) Emission:
- After alpha or beta decay, the nucleus is often left in an excited (high-energy) state. It releases this excess energy as a gamma ray.
- No change in mass or atomic number. The element remains the same.
- Equation:
AZX* → AZX + 00γ(The * indicates an excited nucleus)
5.2.4 Nuclear Fission and Fusion
These are processes that involve changes to the nucleus and release vast amounts of energy, much of it in the form of radiation.
Nuclear Fission:
- The splitting of a large, unstable nucleus into two smaller, more stable nuclei.
- Induced when a free neutron is absorbed by the nucleus (e.g., Uranium-235 or Plutonium-239).
- Releases 2 or 3 more neutrons and a large amount of energy (as gamma radiation and kinetic energy).
- These new neutrons can go on to cause more fission events, leading to a chain reaction.
- Used in nuclear power plants and atomic weapons.
- Fission Equation Example:
23592U + 10n → 9236Kr + 14156Ba + 310n + energy
Nuclear Fusion:
- The joining of two light nuclei to form a heavier nucleus.
- Requires extremely high temperatures and pressures to overcome the electrostatic repulsion between positively charged nuclei.
- The mass of the product nucleus is less than the mass of the original nuclei; the lost mass is converted into a huge amount of energy (primarily as gamma radiation).
- This is the process that powers stars, including the Sun.
- Fusion Equation Example (The Sun):
21H + 31H → 42He + 10n + energy
Key Rule for All Nuclear Equations:
- The sum of the mass numbers (A) must be equal on both sides of the equation.
- The sum of the atomic numbers (Z) must be equal on both sides of the equation.
5.2.5 Half-Life
The half-life of a radioactive isotope is the time taken for half of the radioactive nuclei in a sample to decay, or for its activity (count rate) to fall by half.
- It is constant for a given isotope.
- To find it from a graph, find the time for the count rate to drop from any value to half of that value.
- Always subtract the background count before performing half-life calculations.
Applications of Radioisotopes:
- Smoke Alarms: Use a long-half-life α-emitter (e.g., Americium-241). Smoke absorbs alpha particles, reducing the current and triggering the alarm.
- Medical Tracers & Therapy: Use short-half-life γ-emitters (e.g., Technetium-99m) for imaging. Use intense γ-emitters (e.g., Cobalt-60) to kill cancer cells.
- Sterilisation & Food Irradiation: Use γ-rays to kill bacteria on medical equipment or in food without damaging the packaging.
- Thickness Control: Use β-emitters to monitor the thickness of sheets of material (e.g., paper, metal) during production.
5.2.6 Safety Precautions
Ionising radiation can damage or kill cells and cause mutations (cancer) by breaking DNA molecules.
Safety Protocols:
- Minimize Time: Spend as little time as possible near a source.
- Maximize Distance: Use tongs; keep the source at arm's length. Intensity follows the inverse square law.
- Use Shielding:
- α-particles: Paper, gloves.
- β-particles: Aluminium.
- γ-rays: Thick lead or concrete.
- Safe Storage: Keep sources in a lead-lined box when not in use.
- Disposal: Use isotopes with a short half-life where possible so they quickly become safe.
Abel Masitsa.