Construct · 3 fields · 4 citations
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In optical mineralogy and gemology, dichroism (more generally pleochroism) is the way an anisotropic crystal absorbs light differently depending on the vibration direction of the light relative to the crystal axes, so the stone shows two (or, if trichroic, three) distinct body colours as it is viewed or rotated. Nesse's Introduction to optical mineralogy explains the directional absorption behind it, and Read's Gemmology describes the dichroscope used to split and compare the colours for identification. The referent is direction-dependent selective absorption in a crystal, used to tell gems apart, and it is a different construct from a chemist's circular dichroism or an optician's dichroic mirror.[1][2]
In biophysical spectroscopy, circular dichroism is the difference in how a chiral molecule absorbs left- versus right-circularly polarised light; because this difference depends on three-dimensional shape, the spectrum reports on a protein's secondary structure or a molecule's handedness. Kelly, Jess, and Price's How to study proteins by circular dichroism lays out how the measurement is made and interpreted. The referent is differential absorption of circularly polarised light by chiral matter, a distinct construct from a crystal's directional colour, sharing only the 'two ways of absorbing' root.[3]
In optics, a dichroic filter or mirror is a thin-film interference coating that sharply transmits one band of wavelengths while reflecting another, so it splits light by colour with very little absorption; it is the heart of beam-splitters, colour-separation systems, and many projector and stage optics. Hecht's Optics treats the multilayer interference that produces the effect. The referent here is wavelength-selective reflection by engineered layers, which, despite the shared name, works by interference rather than the selective absorption behind crystal pleochroism or circular dichroism.[4]
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