Beta Decay Simplified Revision Notes for Scottish Highers Physics
Revision notes with simplified explanations to understand Beta Decay quickly and effectively.
Learn about Nuclear Reactions for your Scottish Highers Physics Exam. This Revision Note includes a summary of Nuclear Reactions for easy recall in your Physics exam
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Radioactive Decay: Beta Decay
Introduction
Beta decay is a type of radioactive decay that involves the conversion of a down quark into an up quark within an atomic nucleus.
This transformation leads to the conversion of a neutron into a proton, accompanied by the emission of a beta particle.
Beta Decay Process
In beta decay, a neutron within an unstable nucleus changes into a proton and emits a beta particle.
The beta particle emitted is an electron (e⁻), and it carries away energy as it leaves the atom.
Atomic Structure Changes
Mass Number Change: During beta decay, the mass number (A) of the nucleus remains unchanged because the total number of protons and neutrons remains the same.
Atomic Number Change: The atomic number (Z) of the nucleus increases by one unit (1) because a neutron is converted into a proton.
Chemical Nomenclature
Beta particles are represented with the symbol "e⁻" to indicate their composition as electrons.
Example: Beta Decay of Carbon-14
Carbon-14 (¹⁴C) is a radioactive isotope of carbon with six protons and eight neutrons.
In beta decay, a neutron within the carbon-14 nucleus changes into a proton, resulting in the formation of nitrogen-14 (¹⁴N), which has seven protons and seven neutrons.
The process is accompanied by the emission of a beta particle (electron).
Beta Decay Equation
The beta decay of carbon-14 into nitrogen-14 can be represented by the equation:
¹⁴C → ¹⁴N + e⁻
Radioactive Decay: Beta Decay
In Summary
Beta decay is a type of radioactive decay in which a neutron is converted into a proton, accompanied by the emission of a beta particle (electron).
During beta decay, the mass number (A) remains unchanged, while the atomic number (Z) increases by one unit.
This process plays a crucial role in the decay of certain radioactive isotopes and has significant implications in nuclear physics and radiometric dating.
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