2017
DOI: 10.12681/bgsg.11681
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Comparative Fourier Transform Infrared and X-Ray Powder Diffraction Analysis of Naturally Occurred K-Feldspars

Abstract: Natural K-feldspars from igneous rocks have been examined by means of X-ray powder diffraction (XRPD) and Fourier transform infrared (FTIR) spectroscopy in the spectral

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Cited by 40 publications
(39 citation statements)
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References 10 publications
(17 reference statements)
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“…3. All the samples show a broad, intense absorption band with a maximum at 1030 cm −1 associated with the Si-O stretching vibrations (Theodosoglou et al 2010;Hsiao et al 2017;Sidorenko et al 2018).…”
Section: Fourier Transform Infrared Spectroscopymentioning
confidence: 99%
“…3. All the samples show a broad, intense absorption band with a maximum at 1030 cm −1 associated with the Si-O stretching vibrations (Theodosoglou et al 2010;Hsiao et al 2017;Sidorenko et al 2018).…”
Section: Fourier Transform Infrared Spectroscopymentioning
confidence: 99%
“…The Si O stretching bands in the 1120-1000 cm −1 and the Al O bending at 915 cm −1 are characteristic of aluminosilicate minerals. The doublet at 800-780 cm −1 and the 720-500 cm −1 zone are respectively due to quartz and feldspar admixtures in the clayey material [20][21][22]. The scanning electron microscope SEM) enabled the observation of the platy-like appearance characteristic of kaolinite [23,24] and locally honeycomb aspect of very thin flakes of extremely small particle size, usually observed for smectite and illite [23,25] in the clayey material (Fig.…”
Section: Mineralogymentioning
confidence: 99%
“…The band located at ~429 cm −1 is due to deformation of O–Si–O bond. K–O stretching is observed at around ~467 cm −1 , which is also coupled with Si–O–Si bending vibration . Saikia et al., also, declare that Fe bearing bonds such as Fe–O are located approximately at around ~532 cm −1 .…”
Section: Resultsmentioning
confidence: 94%
“…Absorption at ~776 cm −1 is correlated with Si–O–Si stretching vibration of quartz . Absorptions located in the range of 1000‐1150 cm −1 are ascribed to Si–O stretching vibrations and the maximum absorption, which is seen at around ~1036 cm −1 is due to the stretching vibration of Si–O bonds . At FTIR spectra of minerals, O–H bonds usually fall in the range of 1600‐3700 cm −1 .…”
Section: Resultsmentioning
confidence: 98%