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Journal ArticleDOI

Interpretation of the Kaolinite-Mullite Reaction Sequence from Infrared Absorption Spectra

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TLDR
In this paper, the phases in the kaolinite-mullite reaction sequence were reexamined by ir absorption spectrophotometry, with particular attention paid to the controversial intermediate Al-containing phases.
Abstract
The phases in the kaolinite-mullite reaction sequence were reexamined by ir absorption spectrophotometry. Particular attention was paid to the controversial intermediate Al-containing phases. Amorphous materials were leached from fired kaolinite samples with NaOH to help identify crystalline phases. Metakaolinite partially decomposes, releasing amorphous γ-Al2O3 and SiO2, before the “950°C” exothermic reaction in which metakaolinite is completely decomposed. The resulting spinel-type phase, which is associated with amorphous SiO2 and some poorly crystalline “primary” mullite, is γ-Al203 (crystalline) rather than an Al-Si spinel. There is some evidence, however, that a fraction of the γ-Al2O3, may be an Al-Si spinel. At ≥1100°C secondary mullite therefore forms primarily from the γ-Al2O3/amorphous SiO2 reaction and the recrystallization of primary mullite, whereas excess amorphous SiO2 eventually crystallizes as cristobalite.

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Journal ArticleDOI

Characterization of the Spinel Phase from SiO2-Al2O3 Xerogels and the Formation Process of Mullite

TL;DR: Two kinds of xerogels were prepared by slow and rapid hydrolyses of tetraethoxysilane and aluminum nitrate nonahydrate dissolved in ethanol as discussed by the authors.
Journal ArticleDOI

Sediments exposed to high temperatures: reconstructing pyrotechnological processes in Late Bronze and Iron Age Strata at Tel Dor (Israel)

TL;DR: In this article, the authors used micromorphology, Fourier transform infrared spectrometry (FTIR), X-ray powder diffractometry (XRD), and XRF spectrometers to characterize natural sediments sampled on and in the proximity of the tell and monitor their transformations due to exposure to high temperatures in an oven and in open fires, focusing on the transformations of the clay mineral components of mud-brick materials.
Journal ArticleDOI

Aluminum-27 and Silicon-29 Magic-Angle Spinning Nuclear Magnetic Resonance Study of the Kaolinite-Mullite Transformation

TL;DR: The 27Al and 29Si NMR signal analysis of samples heated above 400°C demonstrates that the tetrahedral sheet of kaolinite begins to break down near 600°C and continues to do so to 900°C as discussed by the authors.
Journal ArticleDOI

29 Si and 27 Al magic-angle-spinning NMR studies of the thermal transformation of kaolinite

TL;DR: The 27Al and 29Si NMR spectra acquired with a 30 s recycle delay of poorly and highly crystalline samples heated at 480 and 500° C, respectively, contain three distinct signals; they discuss their assignment in the light of experiments involving leaching of the samples with aqueous KOH as discussed by the authors.
Journal ArticleDOI

Spinel Phase Formation During the 980°C Exothermic Reaction in the Kaolinite‐to‐Mullite Reaction Series

TL;DR: In this article, it was shown that γ-Al2O3 type spinel phase is solely responsible for the 980°C exotherm in the kaolinite-to-mullite reaction series.
References
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Journal Article

Isomorphous substitution and infra-red spectra of the layer lattice silicates

TL;DR: In this article, the IR spectra of series of dioctahedral and trio-clay clays in the region 400-5000 cm -1 have been obtained.
Journal ArticleDOI

Etude infra-rouge des orthosilicates et des orthogermanates—II: Structures du type olivine et monticellite

TL;DR: In this paper, the authors applied the method of isomorphic substitution to the infra-red spectra of silicates and germanates of the olivine type, and gave a fairly detailed assignment of, and given a description of, the properties of the spectra.
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