Construct · 2 fields · 3 citations
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In physical chemistry, opalescence is the intense, milky scattering of light a fluid shows as it nears its critical point: density or concentration fluctuations grow until they span sizes comparable to the wavelength of light, so the once-clear medium scatters strongly and turns cloudy. Einstein's 1910 Theorie der Opaleszenz von homogenen Flüssigkeiten... derived this critical opalescence from the thermodynamics of fluctuations, linking scattering strength to compressibility. The referent is light scattered by refractive-index fluctuations in a medium, the same physical cause behind the milky glow of an opal.[1]
In gemology, opalescence is the soft, milky, often bluish glow of common opal and other translucent stones, produced when light scatters off sub-microscopic structures and inclusions suspended in the material. Nassau's The physics and chemistry of color places this among the scattering causes of appearance (distinct from the diffraction that gives precious opal its flashing play-of-colour), and Read's Gemmology uses the term for the characteristic turbid sheen. It is the same light-scattering construct as critical opalescence, here fixed permanently in the stone's structure rather than appearing only near a phase transition.[2][3]
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