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near infrared spectra

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Journal Article
Published: 01 July 2010
American Mineralogist (2010) 95 (7): 908–920.
... ; Vervoort et al. 2007 ; Brewer et al. 2008 ), and these may record earlier metamorphic events that predated Belt deposition. Visible and near infrared (Vis/NIR, 350–2500 nm) reflectance spectra were acquired with a FieldSpec FR Pro portable spectroradiometer (Analytical Spectral Devices, Inc...
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Journal Article
Published: 01 July 2005
American Mineralogist (2005) 90 (7): 1209–1212.
...Hans Keppler; Joseph R. Smyth Abstract High pressure optical and near infrared spectra of a single crystal of ringwoodite with composition (Mg 0.90 Fe 0.10 ) 2 SiO 4 were measured to 21.5 GPa. The spectrum at ambient pressure shows a strong band at 12 265 cm −1 with two shoulders at 8678 cm −1...
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Journal Article
Journal: Geology
Published: 01 July 1994
Geology (1994) 22 (7): 621–624.
...Edward F. Duke Abstract Near infrared (NIR) spectra of Precambrian metagraywacke in the Black Hills, South Dakota, demonstrate that reflectance spectroscopy can be used to monitor progressive changes in mineral chemistry as a function of metamorphic grade. The wavelength of a combination Al-O-H...
Journal Article
Journal: Economic Geology
Published: 01 February 1987
Economic Geology (1987) 82 (1): 230–232.
Journal Article
Journal: Economic Geology
Published: 01 February 1987
Economic Geology (1987) 82 (1): 233–234.
Journal Article
Journal: Economic Geology
Published: 01 December 1985
Economic Geology (1985) 80 (8): 2230–2239.
...Gary L. Raines; Linda G. McGee; Stephen J. Sutley Abstract The near-infrared spectra of a suite of outcrop samples of massive sulfide gossans and false gossans representing three different weathering environments were measured and studied with X-ray, scanning electron microscope, and energy...
Journal Article
Published: 01 December 1983
Clays and Clay Minerals (1983) 31 (6): 447–449.
Journal Article
Journal: Geophysics
Published: 01 April 1979
Geophysics (1979) 44 (4): 820–825.
...G. R. Hunt; J. C. Wynn Abstract Bidirectional reflection spectra are presented from 0.35 to 2.5 mu m for a suite of ultramafic rocks collected from chromium-rich areas in southwestern Oregon and northwestern California. Features due to the presence of chromium are entirely absent from these spectra...
Journal Article
Journal: Clay Minerals
Published: 01 December 2000
Clay Minerals (2000) 35 (5): 753–761.
...J. MADEJOVÁ; J. BUJDÁK; S. PETIT; P. KOMADEL Abstract Diffuse reflectance spectra in the near-infrared region are presented for Li-saturated smectites heated up to 200°C. The smectites included three montmorillonites, an Fe-beidellite and a ferruginous smectite. Unheated samples showed a complex...
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Journal Article
Journal: Clay Minerals
Published: 16 March 2022
Clay Minerals (2021) 56 (4): 292–298.
... temperature through their absorption of the visible, near-infrared and far-infrared wavelength regions is evaluated. In particular, the absorption of ultraviolet and infrared radiation by the tiles was evaluated, as this could have beneficial applications for human health and the environment. UV-A radiation...
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Journal Article
Published: 01 February 2016
American Mineralogist (2016) 101 (2): 423–430.
... between the d (06–33) and the Ni/Mg ratio of the synthesized samples following a Vegard’s law and suggested a random distribution of octahedral cations. For the first time, infrared spectra of this series were given in both near and mid-infrared spectral regions (250–7500 cm −1 ). Notably, the bands due...
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Journal Article
Journal: AAPG Bulletin
Published: 11 October 1995
AAPG Bulletin (1995) 79 (10): 1464–1479.
... do not affect the ratio-OM maturity relation substantially. Iron absorption occurs in the short wavelength part of the visible and near-infrared region and is readily identified in the laboratory spectra. Spectra affected by recycled OM were identified by using a pair of ratios that expresses...
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Journal Article
Published: 01 August 1988
Clays and Clay Minerals (1988) 36 (4): 310–316.
Journal Article
Journal: Geophysics
Published: 01 December 1979
Geophysics (1979) 44 (12): 1974–1986.
...G. R. Hunt Abstract Reflection spectra of particulate samples of minerals that commonly occur in hydrothermally altered rocks and soils were recorded to display their features at their natural spectral bandwidths in the near-infrared from 1.3 to 2.4 mu m. Atmospheric transmission spectra were...
Journal Article
Journal: Economic Geology
Published: 01 November 1979
Economic Geology (1979) 74 (7): 1613–1629.
...G. R. Hunt; R. P. Ashley Abstract Visible and near-infrared (0.35 to 2.5 mu m) bidirectional reflection spectra were recorded for a suite of well-characterized hydrothermally altered rock samples. The spectra typically display well-defined bands caused by both electronic and vibrational processes...
Journal Article
Published: 01 December 1957
American Mineralogist (1957) 42 (11-12): 732–742.
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Mid-infrared (a) and near-infrared spectra (b) of clay samples before (TAG) and after the purification treatment (Na+-TAG).
Published: 01 June 2012
Figure 8 Mid-infrared (a) and near-infrared spectra (b) of clay samples before (TAG) and after the purification treatment (Na + -TAG).
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Near infrared spectra of three pantelleritic glasses with total water content, ranging from 2.24 (0.10) to 5.45 (0.10) wt% and sample thickness of 0.0394 to 0.0360 cm. Spectra offset vertically for clarity. In the spectra, the band at 4500 cm–1 is assigned to the combination of stretching and bending of OH group and the band at 5200 cm–1 to the combination of stretching and bending mode of H2O molecules, while the 4000 cm–1 peak is unresolved (see the text).
Published: 01 July 2020
Figure 1. Near infrared spectra of three pantelleritic glasses with total water content, ranging from 2.24 (0.10) to 5.45 (0.10) wt% and sample thickness of 0.0394 to 0.0360 cm. Spectra offset vertically for clarity. In the spectra, the band at 4500 cm –1 is assigned to the combination
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Total water content determined by near-infrared spectra analysis vs. water content measured by KFT. Note that there is a good correlation between the two sets of data determined by different methodologies, both in the case of the GG and TT baseline correction and evaluation of peak height and peak area. Both the 1:1 line and the four equations (and relative R2 values) of the fit lines support the ability to fit the data with constant values of molar absorptivity (discussed further in text).
Published: 01 July 2020
Figure 5. Total water content determined by near-infrared spectra analysis vs. water content measured by KFT. Note that there is a good correlation between the two sets of data determined by different methodologies, both in the case of the GG and TT baseline correction and evaluation of peak
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Decomposition of the near-infrared spectra of samples in which the clay material is composed of (a) 75% smectite–25% kaolinite and (b) 90% smectite–10% kaolinite. See Hébert et al., 2015 for more details on the method of quantification of Sm%.
Published: 27 October 2017
Fig. 9 Decomposition of the near-infrared spectra of samples in which the clay material is composed of (a) 75% smectite–25% kaolinite and (b) 90% smectite–10% kaolinite. See Hébert et al. , 2015 for more details on the method of quantification of Sm%.