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Sediment mineralogy based on visible and near-infrared reflectance spectroscopy
Jarrard, R.D.; Vanden Berg, M.D. (2006). Sediment mineralogy based on visible and near-infrared reflectance spectroscopy, in: Rothwell, R.G. (Ed.) New techniques in sediment core analysis. Geological Society Special Publication, 267: pp. 129-140
In: Rothwell, R.G. (Ed.) (2006). New techniques in sediment core analysis. Geological Society Special Publication, 267. Geological Society: London. ISBN 1-86239-210-2. 266 pp. https://dx.doi.org/10.1144/GSL.SP.2006.267
In: Hartley, A.J. et al. (Ed.) Geological Society Special Publication. Geological Society of London: Oxford; London; Edinburgh; Boston, Mass.; Carlton, Vic.. ISSN 0305-8719; e-ISSN 2041-4927, meer

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  • Jarrard, R.D.
  • Vanden Berg, M.D.

Abstract
    Visible and near-infrared spectroscopy (VNIS) can be used to measure reflectance spectra (wavelength 350-2500 nm) for sediment cores and samples. A local ground-truth calibration of spectral features to mineral percentages is calculated by measuring reflectance spectra for a suite of samples of known mineralogy. This approach has been tested on powders, core plugs and split cores, and we conclude that it works well on all three, unless pore water is present. Initial VNIS studies have concentrated on determination of relative proportions of carbonate, opal, smectite and illite in equatorial Pacific sediments. Shipboard VNIS-based determination of these four components was demonstrated on Ocean Drilling Program Leg 199.

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