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FT-IR Partial Least-Squares Analysis of Tubular Halloysite in Kaolin Samples from the Mount Hope Kaolin Deposit

Published online by Cambridge University Press:  09 July 2018

L J. Janik
Affiliation:
CSIRO Division of Soils, Private Bag 2, Glen Osmond, South Australia and
J. L. Keeling
Affiliation:
Department of Mines & Energy, 191 Greenhill Road, Parkside, Adelaide, South Australia

Abstract

A method of infrared (IR) analysis for quantitative determination of tubular halloysite in mixtures with kaolinite was investigated for drill hole samples collected during an assessment of paper-coating kaolin resources at the Mount Hope Kaolin Deposit, Eyre Peninsula, South Australia. Tubular, dehydrated halloysite from the deposit does not readily intercalate formamide, and the proportion of tubes in <2 μm size-fractions was determined initially from scanning electron micrographs. For samples showing a range of tube contents, a strong correlation between IR spectral response and counts of halloysite tubes was established using partial leastsquares analysis. This provided a rapid technique suitable for routine determination of tubular halloysite in samples from the Mount Hope deposit. Although the universality of the method remains to be tested, it offers an alternative approach to other analytical techniques for assessment of kaolin deposits where the presence of halloysite is suspected.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1993

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References

Bailey, S.W. (1990) Halloysite—a critical assessment. Proc. 9th Int. Clay Conf., Strasbourg, 8998.Google Scholar
Bates, T.F., Hilderbrand, F.A. & Swineford, A. (1950) Morphology and structure of endellite and halloysite. Am. Miner. 35, 463484.Google Scholar
Brindley, G.W., Souza Santos, P. de. & Souza Santos H. de. (1963) Mineralogical studies of kaolinite-halloysite clays: I. Identification problems. Am. Miner. 48, 897910.Google Scholar
Bristow, C.M. (1987) World kaolins: genesis, exploitation and application. Industrial Minerals, July 1987, 4559.Google Scholar
Churchman, G.J. & Gilkes, R.J. (1989) Recognition of intermediates in the possible transformation of halloysite to kaolinite in weathering profiles. Clay Miner. 24, 579590.Google Scholar
Churchman, G.J., Witton, J.S., Claridge, G.G.C. & Theng, B.K.G. (1984) Intercalation method using formamide for differentiating halloysite from kaolinite in weathering profiles. Clays Clay Miner. 32, 241248.Google Scholar
Crowley, J.K & Vergo, N. (1988) Near-infrared reflectance spectra of mixtures of kaolin-group minerals: use in clay mineral studies. Clays Clay Miner. 36, 310316.CrossRefGoogle Scholar
Dixon, J.B. (1989) Kaolin and serpentine group minerals. Pp. 467-525 in: Minerals in Soil Environments. (J.B. Dixon & S.B. Weed, editors) Soil Sci. Soc. Am., Madison, Wisconsin, USA.Google Scholar
Farmer, V.C. & Russell, J.D. (1964) The infrared spectra of layer silicates. Spectrochim. Acta 20, 11491173.Google Scholar
Haaland, D.M. & Thomas, V.T. (1988a) Partial Least-squares methods for spectral analyses. 1. Relation to other quantitative calibration methods and the extraction of qualitative information. Anal. Chem. 60, 11931202.Google Scholar
Haaland, D.M. & Thomas, V.T. (1988b) Partial Least-squares methods for spectral analyses. 2. Application to simulated and glass spectral data. Anal. Chem. 60, 12021208.Google Scholar
Hasofer, A.M. (1963) On the reliability of the point-counter method in petrography. Aust. J. Appl. Sci. 14, 168179.Google Scholar
Keeling, J.L., Self, P.G., McClure, S.G., Raven, M.D. & Milnes, A.R. (1992) Characterisation of kaolin samples from the Mount Hope deposit, Eyre Peninsula, South Australia. South Australia, Mines & Energy Review 158, 2126.Google Scholar
Nguyen, T.T., Janik, L.J. & Raupach, M. (1991) Diffuse Reflectance Infrared Fourier Transform (DRIFT) spectroscopy in soil studies. Aust. J. Soil Res. 29, 4967.Google Scholar
Solomon, M. (1963) Counting and sampling errors in modal analysis by point-counter. J. Pet. 4, 367382.Google Scholar
Solomon, M. & Green, R. (1965) A chart for designing modal analysis by point counting. Geol. Runds. 55, 844-848.Google Scholar
Theng, B.K.G., Chruchman, G.J., Witton, J.S. & Claridge, G.G.C. (1984) Comparison of intercalation methods for differentiating halloysite from kaolinite. Clays Clay Miner. 32, 249259.CrossRefGoogle Scholar
Thomas, V.T. & Haaland, D.M. (1990) Comparison of multivariate calibration methods for quantitative spectral analysis. Anal. Chem. 62, 10911099.Google Scholar
Van der Marel, H.W. & Beutelspacher, H. (1976) Clay-and related minerals: Kaolin minerals (kandites). Pp. 6589 in: Atlas of Infrared Spectroscopy of Clay Minerals and their Admixtures. (H.W. van der Marel & H. Beutelspacher, editors.) Elsevier, Amsterdam.Google Scholar