Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-05T04:35:11.015Z Has data issue: false hasContentIssue false
  • English
  • Français

Mid-Infrared Features of Kaolinite-Dickite

Published online by Cambridge University Press:  01 January 2024

Javier Cuadros ,
Raquel Vega  and
Alejandro Toscano
Javier Cuadros*
Affiliation:
Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK
Raquel Vega
Affiliation:
Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK
Alejandro Toscano
Affiliation:
Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK
*
*E-mail address of corresponding author: [email protected]
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Transformation of kaolinite to dickite is a common diagenetic reaction. The present report is part of a wider study to investigate the pathways of this polytype change. Fourier-transform infrared spectroscopy (FTIR) was used to attempt quantification of the relative proportions of kaolinite and dickite, validated by X-ray diffraction (XRD) results, in order to link mineral and structural features during the mineralogical changes. A group of kaolinite and dickite samples was investigated: 13 samples from the Frøy and Rind oil fields (North Sea), three kaolinite specimens with different crystal order and particle size (KGa-2, kaolinite API 17, Keokuk kaolinite), and two dickite-rich samples (Natural History Museum collection). Six FTIR spectral features were analyzed: (1) intensity ratio of the minima at 3675 and 3635 cm−1; (2) position of the band at ~1115 cm−1; (3) difference between the frequency of the bands at ~1030 and ~1000 cm−1; (4) intensity ratio of the bands generating shoulders at ~922 and ~900 cm−1; (5) position of the band at ~370 cm−1; and (6) intensity of the band at ~268 cm−1. Correlation of the features above with polytype relative proportions derived from XRD showed non-linear behavior, with maximum curvature at the dickite end, which precludes kaolinite-dickite quantification. Increasing kaolin particle size is known to cause decreased intensity of the FTIR spectra. A model was developed to test whether this effect is consistent with the non-linear progression of the IR features. The relative intensity of kaolinite and dickite IR features were calculated in a series of kaolinite-to-dickite transformations, where the size of particles increases with dickite proportion, and where dickite-dominated particles reach a larger size than kaolinite-dominated particles. The results indicated that the differential particle size increase is possibly the cause of the lack of linearity between IR- and XRD-measured dickite proportions.

Keywords

DickiteInfrared SpectroscopyKaolinite
Type
Research Article
Information
Clays and Clay Minerals , Volume 63 , Issue 2 , April 2015 , pp. 73 - 84
Copyright
Copyright © Clay Minerals Society 2015

References

Anovitz, L.M. Perkins, D. and Essene, E.J., 1991 Metastability in near-surface rocks in the system Al2O3-SiO2-H2O Clays and Clay Minerals 39 225–233.CrossRefGoogle Scholar
Balan, E. Saitta, A. Mauri, F. and Calas, G., 2001 First-principles modeling of the infrared spectrum of kaolinite American Mineralogist 86 1321–1330.CrossRefGoogle Scholar
Balan, E. Refson, K. Blanchard, M. Delattre, S. Lazzeri, M. Ingrin, J. Mauri, F. Wright, K. and Winkler, B., 2008 Theoretical infrared absorption coefficient of OH groups in minerals American Mineralogist 93 950–953.CrossRefGoogle Scholar
Balan, E. Delattre, S. Guillaumet, M. and Salje, E., 2010 Low-temperature infrared spectroscopic study of OH-stretching modes in kaolinite and dickite American Mineralogist 95 1257–1266.CrossRefGoogle Scholar
Bassan, P. (2011) Light scattering during infrared spectroscopic measurements of biomedical samples. PhD thesis, University of Manchester, UK, 120 pp.Google Scholar
Beaufort, D. Cassagnabère, A. Petit, S. Lanson, B. Berger, G. Lacharpagne, J.C. and Johansen, H., 1998 Kaolinite to dickite reaction in sandstone reservoirs Clay Minerals 33 297–316.CrossRefGoogle Scholar
Benco, L. Tunega, D. Hafner, J. and Lischka, H., 2001 Orientation of OH groups in kaolinite and dickite: Ab initio molecular dynamics study American Mineralogist 86 1057–1065.CrossRefGoogle Scholar
Brindley, G.W. Kao, C.-C. Harrison, J.L. Lipsicas, M. and Raythatha, R., 1986 Relation between structural disorder and other characteristics of kaolinites and dickites Clays and Clay Minerals 34 239–249.CrossRefGoogle Scholar
Cassagnabère, A. (1998) Caracterisation et interpretation de la transition kaolinite-dickite dans les reservoirs a hydrocarbures de Froy et Rind (Mer du Nord), Norvege. PhD thesis, Université de Poitiers, France, 214 pp.Google Scholar
Cuadros, J. Vega, R. Toscano, A. and Arroyo, X., 2014 Kaolinite transformation into dickite during burial diagenesis American Mineralogist 99 681–695.CrossRefGoogle Scholar
Dahm, D.J. Dahm, K.D., Williams, P.W. and Norris, K., 2001 The physics of nearinfrared scattering Near-Infrared Technology in the Agricultural and Food Industries St. Paul Minnesota, USA American Association of Cereal Chemists.Google Scholar
De Ligny, D. and Navrotsky, A., 1999 Energetics of kaolin polymorphs American Mineralogist 84 506–516.CrossRefGoogle Scholar
Farmer, V.C., Farmer, V.C., 1974 The layer silicates The Infrared Spectra of Minerals London Mineralogical Society.CrossRefGoogle Scholar
Farmer, V.C., 1998 Differing effects of particle size and shape in the infrared and Raman spectra of kaolinite Clay Minerals 33 601–604.CrossRefGoogle Scholar
Farmer, V.C., 2000 Transverse and longitudinal crystal modes associated with OH stretching vibrations in single crystals of kaolinite and dickite Spectrochimica Acta Part A 56 927–930.CrossRefGoogle ScholarPubMed
Farmer, V.C. and Russell, J.D., 1964 The infrared spectra of layer silicates Spectrochimica Acta 20 1149–1173.CrossRefGoogle Scholar
Farmer, V.C. and Russell, J.D., 1966 Effects of particle size and structure on the vibrational frequencies of layer silicates Spectrochimica Acta 22 389–398.CrossRefGoogle Scholar
Fialips, C.I. Navrotsky, A. and Petit, S., 2001 Crystal properties and energetics of synthetic kaolinite American Mineralogist 86 304–311.CrossRefGoogle Scholar
Fialips, C.-I. Majzlan, J. Beaufort, D. and Navrotsky, A., 2003 New thermochemical evidence on the stability of dickite vs. kaolinite American Mineralogist 88 837–845.CrossRefGoogle Scholar
Frost, R., 1997 The structure of the kaolinite minerals — a FT-Raman study Clay Minerals 32 65–77.CrossRefGoogle Scholar
Frost, R.L., 1998 Hydroxyl deformation in kaolins Clays and Clay Minerals 46 280–289.CrossRefGoogle Scholar
Hayes, J.B., 1936 Kaolinite from Warsaw geodes, Keokuk Region, Iowa Iowa Academy of Sciences Proceedings 70 261–272.Google Scholar
Johnston, C. Kogel, J. Bish, D. Kogure, T. and Murray, H., 2008 Low-temperature FTIR study of kaolin-group minerals Clays and Clay Minerals 56 470–485.CrossRefGoogle Scholar
Kerr, P.F. and Kulp, J.L., 1949 Reference clay localities — United States American Petroleum Institute, Project 49, Clay Mineral Standards, Preliminary Report no. 2, 24–25 New York Columbia University.Google Scholar
King, P.L., Ramsey, M.S., McMillan, P.F., and Swayze, G. (2004) Laboratory Fourier transform infrared spectroscopy methods for geological samples. Pp. 57–92 in: Infrared Spectroscopy in Geochemistry, Exploration Geochemistry and Remote Sensing (King, P.L., Ramsey, M.S., and Swayze, G.A., editors). Mineralogical Association of Canada.Google Scholar
Kogure, T. and Inoue, A., 2005 Stacking defects and longperiod polytypes in kaolin minerals from a hydrothermal deposit European Journal of Mineralogy 17 465–473.CrossRefGoogle Scholar
Kogure, T. and Inoue, A., 2005 Determination of defect structures in kaolin minerals by high-resolution transmission electron microscopy (HRTEM) American Mineralogist 90 85–89.CrossRefGoogle Scholar
Lanson, B. Beaufort, D. Berger, G. Bauer, A. Cassagnabère, A. and Meunier, A., 2002 Authigenic kaolin and illitic minerals during burial diagenesis of sandstones: a review Clay Minerals 37 1–22.CrossRefGoogle Scholar
Lindberg, J.D. and Smith, M.S., 1974 Visible and near infrared absorption coefficients of kaolinite and related clays American Mineralogist 59 274–279.Google Scholar
Lombardi, G. Russell, J.D. and Keller, W.D., 1987 Composition and structural variations in the size fractions of a sedimentary and a hydrothermal kaolin Clays and Clay Minerals 35 321–335.CrossRefGoogle Scholar
Mermut, A.R. and Cano, A.F., 2001 Baseline studies of the Clay Minerals Society Source Clays: chemical analyses of major elements Clays and Clay Minerals 49 381–386.CrossRefGoogle Scholar
Moll, W. Jr, 2001 Baseline studies of the Clay Minerals Society Source Clays: Geological origin Clays and Clay Minerals 49 374–380.CrossRefGoogle Scholar
Prost, R. Dameme, A. Huard, E. Driard, J. and Leydecker, J.P., 1989 Infrared study of structural OH in kaolinite, dickite, nacrite, and poorly crystalline kaolinite at 5 to 600 K Clays and Clay Minerals 37 464–468.CrossRefGoogle Scholar
Robin, V. Petit, S. Beaufort, D. and Prêt, D., 2013 Mapping kaolinite and dickite in sandstone thin sections using infrared microspectroscopy Clays and Clay Minerals 61 141–151.CrossRefGoogle Scholar
Russell, J.D. Fraser, A.R., Wilson, M.J., 1994 Infrared methods Clay Mineralogy: Spectroscopic and Chemical Determinative Methods London Chapman & Hall.Google Scholar
Sato, H. Ono, K. Johnston, C. and Yamagishi, A., 2004 First-principle study of polytype structures of 1:1 dioctahedral phyllosilicates American Mineralogist 89 1581–1585.CrossRefGoogle Scholar
Shoval, S. Yariv, S. Michaelian, K. Boudeulle, M. and Panczer, G., 1999 Hydroxyl-stretching bands ‘A’ and ‘Z’ in Raman and infrared spectra of kaolinites Clay Minerals 34 551–563.CrossRefGoogle Scholar
Shoval, S. Yariv, S. Michaelian, K. Boudeulle, M. and Panczer, G., 2002 Hydroxyl-stretching bands in polarized micro-Raman spectra of oriented single-crystal Keokuk kaolinite Clays and Clay Minerals 50 56–62.CrossRefGoogle Scholar
van der Marel, H.V. and Beutelspacher, H., 1976 Atlas of Infrared Spectroscopy of Clay Minerals and their Admixtures Amsterdam Elsevier.Google Scholar
Zimmerle, W. and Rösch, H., 1990 Petrogenetic significance of dickite in European sedimentary rocks Zentralblatt für Geologie und Paläontologie Teil I 1175–1196.Google Scholar