Nuclear Radiation and Radioactive Decay
This section explores nuclear radiation and radioactive decay, crucial topics in AQA GCSE Physics topic 4 Atomic Structure.
Radioactive decay occurs when an unstable nucleus of an isotope stabilizes by emitting radiation. This process is entirely random and unpredictable for individual atoms.
Definition: Activity in radiation refers to the rate at which a source of unstable nuclei decays, measured in Becquerels (Bq).
1 Becquerel equals 1 decay per second, typically measured using a Geiger-Muller tube. The count rate, which is the number of decays recorded each second by a detector, is also measured using a Geiger-Muller tube.
There are four main types of radiation:
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Alpha particles:
- Travel 5cm in air before stopping
- Stopped by paper
- Highly ionizing
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Beta particles:
- Can reach 15cm in air
- Stopped by a few mm of aluminum
- Quite strongly ionizing
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Gamma rays:
- Travel several meters in air
- Require several cm of lead to stop
- Weakly ionizing
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Neutron radiation (not detailed in this transcript)
Highlight: During beta decay, a neutron changes into a proton and emits a fast-moving electron, which becomes the beta particle.
Ionization is the process where an electron gains enough energy to break away from an atom. This concept is crucial in understanding the effects of radiation on matter.