Constituents of the atom (AQA A-Level Physics): Revision Notes
📚 Revision Notes
2.1.1 Constituents of the atom
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Atoms are composed of three fundamental particles: protons, neutrons, and electrons.
- Protons and neutrons are found in the nucleus at the centre of an atom and are collectively known as nucleons.
- Electrons orbit the nucleus in regions called shells or energy levels. Each of these particles has unique properties, which can be measured in SI units (Standard International units) and relative units. A summary of these properties is presented below:
| Particle | Charge (Coulombs) | Relative Charge | Mass (kg) | Relative Mass | Specific Charge (C/kg) |
|---|---|---|---|---|---|
| Proton | +1 | 1 | |||
| Neutron | 0 | 0 | 1 | 0 | |
| Electron | -1 | 0.0005 |
Specific Charge
Specific charge is a measure of the charge-to-mass ratio of a particle. It is calculated by dividing the particle's charge by its mass.
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Example Calculation
For a proton, with a charge of and a mass of kg:
This calculation shows the specific charge value, which is useful for comparing different particles' behaviour in electric and magnetic fields.
Atomic Notation and Definitions
- Proton Number (): The number of protons in an atom. This defines the element's identity (e.g., Hydrogen has ( ), Carbon has ( ).
- Nucleon Number (A): The total number of protons and neutrons in the nucleus. It represents the mass number and gives an approximation of the atom's mass.
- Nuclide Notation: A specific way of representing atoms using the form , where:
- = Nucleon number,
- = Proton number,
- = Element symbol.
Isotopes and Carbon Dating
Isotopes are variants of the same element that have the same number of protons but different numbers of neutrons. This difference in neutron count leads to different mass numbers for isotopes of the same element.
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Example: Carbon-
- Carbon- is a radioactive isotope of carbon, used in carbon dating to determine the age of organic materials.
- Carbon dating process: By measuring the remaining percentage of Carbon- in a sample and knowing its half-life (the time it takes for half of a sample to decay), scientists can estimate the age of objects containing organic material, such as archaeological artefacts.