2002
DOI: 10.1029/2000je001467
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Spectral reflectance properties of zeolites and remote sensing implications

Abstract: [1] The 0.3-to 26-mm reflectance spectra of a suite of 28 zeolites were measured and analyzed to derive spectral-compositional-structural relationships. Below $7 mm, the spectra are largely dominated by absorption features associated with zeolitic water. At longer wavelengths, the spectra are dominated by absorption features associated with the aluminosilicate framework. The spectra exhibit a number of systematic variations which can be used for both structural and compositional determinations. These include: … Show more

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Cited by 53 publications
(53 citation statements)
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“…The drop in the transmitted intensity for the dry, water, and ice spectra at 1650-1700 nm shown in Figs. 3(a) and 3(b) (water and ice alone) can be attributed to first-order overtones and combinations of various C-H stretching fundamentals [8] that appear distinctively for asphalts with high bitumen content. This also affects the transparent media water and ice, so this is not an effect of spectrometer.…”
Section: Discussionmentioning
confidence: 99%
“…The drop in the transmitted intensity for the dry, water, and ice spectra at 1650-1700 nm shown in Figs. 3(a) and 3(b) (water and ice alone) can be attributed to first-order overtones and combinations of various C-H stretching fundamentals [8] that appear distinctively for asphalts with high bitumen content. This also affects the transparent media water and ice, so this is not an effect of spectrometer.…”
Section: Discussionmentioning
confidence: 99%
“…ROI A06_001 lies within the high albedo bright-toned unit, and exhibits a flat spectrum with no absorption features (Fig. 6C), potentially indicative of alteration minerals such as gypsum, opaline silica, zeolites, or magnesium sulfate (Hunt and Ashley, 1979;Cloutis et al, 2002;Ehlmann et al, 2012). The AUPE-2 R ⁄ spectra for this ROI accurately captured this spectral profile at all wavelengths as identified with the corresponding spectrometer field measurement except for the 440 nm value.…”
Section: Contextual Mineralogy and Field Observationsmentioning
confidence: 94%
“…Extrinsic absorption in the polymer is due to external impurities like absorbed water. This can be detected by spectroscopy analysis as changes in hydroxyl (O-H) peaks at 1400 and 1900 nm [10], [11]. The overlap of the tails of different absorption peaks makes the contribution of absorption loss significant to the overall optical loss of the waveguide.…”
Section: Optical Loss Mechanismsmentioning
confidence: 99%