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• W2058906536 abstract "Summary The reliability and utility of diffuse reflectance spectra are briefly but critically reviewed. The results of measurements of diffuse reflectance over the wavelength range 200 < λ < 2500 nm are reported for wüstite, magnetite, hematite, maghemite, ilmenite, ulvöspinel, and α -FeO · OH (goethite), β -FeO 7sd OH, γ -FeO · OH (lepidocrocite), and δ -FeO · OH. The spectra have been assigned by reference to simplified molecular-orbital energy-level diagrams derived from recent SCF-X α calculations. The specular reflectances reported in the Quantitative Data File (Henry, 1977) are related to the diffuse reflectance spectra in a rational way. Minerals that absorb strongly throughout the visible display little dispersion of specular reflectance, and their powders are dark (wüstite, magnetite, ilmenite, ulvöspinel); those that absorb much more strongly in the near ultraviolet than in the visible have specular reflectances that decrease monotonically from blue to red according to a simple dispersion relation derived by combining the Sellmeier dispersion and Fresnel reflexion equations; their powders are strongly coloured (hematite, maghemite, lepidocrocite, goethite) and their optical anisotropy is closely related to crystal structure." @default.
• W2058906536 created "2016-06-24" @default.
• W2058906536 creator A5037437100 @default.
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• W2058906536 date "1979-09-01" @default.
• W2058906536 modified "2023-10-17" @default.
• W2058906536 title "Diffuse reflectance spectra and optical properties of some iron and titanium oxides and oxyhydroxides" @default.
• W2058906536 cites W1674010494 @default.
• W2058906536 cites W2016374834 @default.
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• W2058906536 doi "https://doi.org/10.1180/minmag.1979.043.327.06" @default.
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