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Dielectric Constant and Polarization

V Background information and definitions
V Polarization and polarizability
V Refractive index
link Water and microwaves
link Complex dielectric permittivity
link Dielectric spectroscopy

Background information and definitions

The electric dipole moment (μ) of a molecule is directed from the center of negative charge (-q) to the center of positive charge (+q) distance r away. The units are usually given in Debye (= 3.336 x 10-30 A s m).

 

μ = qr

 

In liquid water, molecules possess a distribution of dipole moments (range ~1.9 - 3.1 D) due to the variety of hydrogen bonded environments.

 

If two charges q1 and q2 are separated by distance r, the (Coulomb) potential energy is V (joule)

 

V = (q1 x q2)/(4 x pi x vacuum permittivity x r)

 

where ε0 is the permittivity of a vacuum (= 8.854 x 10-12 C2 J-1 m-1; the ability of a material to store electrostatic energy).

 

In a medium it is lower

 

where ε is the medium's permittivity.

V = (q1 x q2)/(4 x pi x medium permittivity x r)

 

The dielectric constant (εr) of the medium (also known as the relative permittivity) is defined as

 

Dielectric constant=medium permittivity/vacuum permittivity

 

and clearly approaches unity in the dilute gas state. In liquid water, it is proportional to the mean-square fluctuation in the total dipole moment. In liquid water, the dielectric constant is high and there is a linear correlation between it and the number of hydrogen bonds [239]. [Back to Top to top of page]

Polarization and polarizability

The polarization (P) of a substance is its electric dipole moment density (see also). The charge density vector (D) is the sum of the effect of the applied field and the polarization.

D = ε0E + P

 

But as

 

D = εE

P = (εr - 1)ε0E

 

The dielectric constant (εr) is related to the molar polarization of the medium (Pm) using the Debye equation

 

(Dielectric constant -1)/(Dielectric constant +2) = mass density x molar polarization/molar mass

 

where ρ is the mass density (kg m-3), M is the molar mass (kg). At high dielectric constant, such as water, the left hand side of the above equation approximates to unity and the molar polarization (calculated from equation(1) below = 181.5x10-6 m3 at 25°C) should approximate to the molar volume (18.0685x10-6 m3 at 25°C) but it clearly does not in the case of water. The molar polarization of the medium (Pm) is defined as

 

Molar polarization = (Avogadro number/(3 x vacuum permittivity)) x (polarizability +(dipole moment squared/(3 x Boltzman constant x temperature))            (1)

 

where α is the polarizability of the molecules, which is the proportionality constant between the induced dipole moment μ* and the field strength E (μ* = αE), NA is the Avogadro number, Mk is the Boltzmann constant (=R/NA), T is the absolute temperature and μ is permanent dipole moment. Unfortunately, in line with many other anomalies of water, this equation is not a good predictor for the behavior of water, which shows a minimum molar polarization at about 15°C. The term in (εr + 2) comes from the relationship between the local field (E') and the applied field (E). 

 

E' = (E/3)(εr + 2) 

 

The polarizability (α) may be given as the polarizability volume (α´) where

 

polarizability volume = polarizability/(4 x pi x vacuum permittivity)

 

The second term in equation (1) is due to the contribution from the permanent dipole moment, which is negligible when the medium is non-polar or when the frequency of the applied field is sufficiently high that the molecules do not have time to change orientation. In this case the Clausius-Mossotti equation holds (but again not for water):

 

(Dielectric constant -1)/(Dielectric constant +2) = mass density x Avogadro number x polarization/(3 x molar mass x vacuum permittivity)

[Back to Top to top of page]   

Refractive index

 

The refractive index (ηr) in the visible and ultraviolet is the ratio of the speed of light in a vacuum (c) to that in the medium (c´); ηr = c/c´. It is also related to the relative permittivity (εr), the absorption coefficient (α) and wavelength (λ) [177].

 

(refractive index)squared equals relative permittivity + (wavelength times absorption coefficient)/(4 times pi)

 

This reduces to ε = ηr2 where ε is the relative permittivity at visible frequencies (4x1014 - 8x1014 Hz, ηr ~ 1.34) and εS = ηr2 where εS is the relative permittivity at low frequencies (static region; < 109 Hz, ηr ~ 9). It also follows that, as the temperature is raised, εr tends towards ηr2 [423]. [Back to Top to top of page]

 

 

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This page was last updated by Martin Chaplin on 25 June, 2008


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