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dielectric permittivity

Dielectric permittivity (ε) characterizes the ability of a medium to polarize under an electric field and weaken it. In vacuum, the electric constant ε₀ ≈ 8.85·10⁻¹² F/m. The relative permittivity εᵣ = ε/ε₀ shows how many times weaker the interaction of charges in the medium is compared to vacuum. For water, εᵣ ≈ 80, which explains water's high dissolving power for ionic compounds.

History

The concept arose from Michael Faraday's experiments in the 1830s, who noticed that more charge accumulated between the plates of a capacitor with a dielectric. The term 'dielectric permittivity' was introduced by William Thomson (Lord Kelvin). Later, James Clerk Maxwell included it in his equations, linking it with the refractive index.

How it works

An electric field tends to align molecules of the substance, especially polar ones (e.g., water), into chains along the field. These aligned molecules create their own weak field directed opposite to the external field, weakening it. The easier the molecules turn, the stronger the weakening, i.e., the higher the permittivity.

💡 Thanks to the huge dielectric permittivity of water (about 80 at room temperature), table salt readily dissolves into ions — water seems to pull the ions apart, weakening their bond by a factor of 80.
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Scientists
James Clerk Maxwell
Related tags
critical pointelectric fieldelectromagnetic radiationpolarizationspeed of light
Laws
Coulomb's law

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