Fourier-transform infrared spectroscopic characterization of naturally occurring glassy fulgurites

We report here for the first time the spectroscopic characterization of natural fulgurites of Garuamukh. On April 22, 2005 at 04:00 local time, large amounts of black-brown colour of colloidal solution came out from below the earth’s surface at Garuamukh near Nagaon town (latitude 26°20′39″N, longit...

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Veröffentlicht in:Bulletin of materials science 2008-04, Vol.31 (2), p.155-158
Hauptverfasser: Saikia, B. J., Parthasarathy, G., Sarmah, N. C., Baruah, G. D.
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container_issue 2
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container_title Bulletin of materials science
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creator Saikia, B. J.
Parthasarathy, G.
Sarmah, N. C.
Baruah, G. D.
description We report here for the first time the spectroscopic characterization of natural fulgurites of Garuamukh. On April 22, 2005 at 04:00 local time, large amounts of black-brown colour of colloidal solution came out from below the earth’s surface at Garuamukh near Nagaon town (latitude 26°20′39″N, longitude 92°41′39″E, Assam, India) with fire and smoke. This colloidal solution got transformed into fulgurites, glassy material, within a few hours. We present here the characterization of the fulgurites by Fourier transform infrared (FTIR) absorption, X-ray diffraction and X-ray fluorescence methods. The amorphous nature of the substance has been confirmed by Fourier transform infrared spectra of the fulgurites, which exhibit prominent absorption band in the region 400–1200 cm −1 , the basic component of amorphous silica. The present study might have significant implications in understanding the thermodynamic properties of naturally occurring glasses, which are formed by shock metamorphism.
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subjects Absorption spectra
Chemistry and Materials Science
Colloids
Engineering
Fourier transforms
Fulgurite
Glassy
Infrared
Infrared spectra
Infrared spectroscopy
Materials Science
Shock metamorphism
Smoke
Spectroscopy
Spectrum analysis
Thermodynamic properties
X-ray fluorescence
X-rays
title Fourier-transform infrared spectroscopic characterization of naturally occurring glassy fulgurites
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