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Beta decay is the most common type of radioactive decay, observed in over 97% of all known unstable nuclides.
It is where a nucleus transforms by emitting a beta particle (an electron or anti-electron) and an antineutrino or neutrino.
There are 3 Types of Beta Decay.
1. β⁻ Decay (Electron Emission)
A neutron converts into a proton, emitting an electron and an electron-antineutrino. The atomic number increases by 1, mass number unchanged.
2. β⁺ Decay (Positron Emission)
A proton converts into a neutron, emitting an anti-electron and an electron-neutrino. The atomic number decreases by 1.
3. Electron Capture
A proton-rich nucleus absorbs an inner-shell electron, which combines with a proton to form a neutron and emit a neutrino.
Examples
| Type | Parent Isotope | Decay Equation | Daughter Isotope | Half-life |
|---|---|---|---|---|
| β⁻ | Carbon-14 | Nitrogen-14 | 5,730 years | |
| β⁻ | Strontium-90 | Yttrium-90 | 29 years | |
| β⁺ | Carbon-11 | Boron-11 | 20 minutes | |
| β⁺ | Fluorine-18 | Oxygen-18 | 110 minutes | |
| Electron capture | Potassium-40 | Argon-40 | 1.25 billion years |
Practical Applications
- Radiocarbon dating – Carbon-14 beta decay measures the age of organic artifacts.
- PET scans – Positron-emitting isotopes like Fluorine-18 annihilate with electrons, producing gamma rays for medical imaging.
- Nuclear reactors – Beta decay of fission products produces delayed neutrons essential for reactor control.
- Betavoltaic batteries – Beta particles generate electricity in long-lasting pacemaker batteries.
Unit 2
Gamma Decay
Unit 4
Alpha Decay
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