Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-19T22:48:22.014Z Has data issue: false hasContentIssue false

The Influence of analytical error upon the interpretation of chemical variations in clay minerals

Published online by Cambridge University Press:  09 July 2018

E. A. Warren
Affiliation:
Centre de Geochimie de la Surface, CNRS 67084 Strasbourg Cedex, France
B. Ransom
Affiliation:
Centre de Geochimie de la Surface, CNRS 67084 Strasbourg Cedex, France

Abstract

Understanding the chemical variability of clay minerals depends on the analytical reliability of the techniques used. Uncertainties in clay mineral compositions were computed for common sources of analytical error such as those that arise from contaminant phases present in clay size-fractions in concentrations below the detection limit of routine XRD screening techniques, and the analytical limits of precision for TEM/AEM analysis. When plotted on standard diagrams used to represent clay mineral compositions, the calculated error envelopes were found to be of significant size, such that analyses of pure illites and pure smectites straddled the field for mixed-layered illite-smectites. In addition, on some diagrams random analytical errors resulted in linear trends identical to those caused by mixtures of two or more clay minerals. It follows that variations in the compositions of clay minerals reported in the literaure do not always necessarily represent the actual chemical variation of the minerals. As a result, current interpretations of clay compositional variations may not be as definitive as hoped.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1992

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Ahn, J.H. & Peacor, D.R. (1986) Transmission and analytical electron microscopy of the smectite-to-illite transition. Clays Clay Miner., 34, 165–188.Google Scholar
Ahn, J.H. & Peacor, D.R. (1989) Illite/smectite from Gulf Coast shales: A reappraisal of transmission electron microscope images. Clays Clay Miner., 37, 542–546.Google Scholar
Buatier, M., Honnorez, J. & Ehret, G. (1989) Fe-smectite-glauconite transition in hydrothermal green clays from the Galapagos Spreading Center. Clays Clay Miner., 37, 532–541.Google Scholar
Butler, J.C. (1979) Trends in ternary petrologic variation diagrams—Fact or fantasy. Am. Miner., 64, 11151121.Google Scholar
Cliff, G. & Lorimer, G.W. (1975) The quantitative analysis of thin specimens 203, 203–207.Google Scholar
Curtis, C.D., Hughes, C.R., Whiteman, J.A. & Whittle, K. (1985) Compositional variation within some chlorites and some comments on their origin. Mineral. Mag., 49, 375–386.Google Scholar
Dudoignon, P., Beaufort, D. & Meunier, A. (1988) Hydrothermal and supergene alterations in the granitic cupola of Montebras, Creuse, France. Clays Clay Miner., 36, 505–520.CrossRefGoogle Scholar
Duplay, J. (1984) Analyses chimiques ponctuelles de particules d'argiles. Relations entre variations de compositions dans une population de particles et temperature de formation Sci. Geol. Bull., 37, 307–317.Google Scholar
Duplay, J., Desprairies, A., Paquet, H. & Millot, G. (1986) Celadonites et glauconites. Double population de particules dans la celadonite de Chypre. Essai sur les temperatures de formation. C.R. Acad. Sc. Paris, 302, Serie II, 181186.Google Scholar
Earley, J.W., Osthaus, B.B. & Milne, I.H. (1953) Purification and properties of montmorillonite. Am. Miner., 38, 707–724.Google Scholar
Foster, M.D. (1954) The relation between "illite:, beideliite, and montmorillonite. 2, 386397.Google Scholar
Giaramita, M.J. & Day, H.W. (1990) Error propagation in calculations of structural formulas. Am. Miner. IS,, 170182.Google Scholar
Giressf, P., Wiewiora, A. & Lacka, B. (1988) Mineral phases and processes within green peloids from two Recent deposits near the Congo River mouth. Clay Miner., 23, 447458.Google Scholar
Goldstein, J.I., Williams, D.B. & Cliff, G. (1987) Quantitative X-ray microanalysis. Pp. 155-218 in: Principles of Analytical Electron Microscopy(D.C. Joy, Romig, A.D. Jr. & Goldstein, J.I., editors). Plenum Press, London.Google Scholar
Goodman, B.A., Nadeau, P.H. & Chadwick, J. (1988) Evidence for the multiphase nature of bentonites from Mossbauer and EPR spectroscopy. Clay Miner., 23, 147–159.Google Scholar
Grim, R.E. & Kulbicki, G. (1961) Montmorillonite: High temperature reactions and classification. Am. Miner., 4 , 13291369.Google Scholar
Hower, J. & MowattT.C, (1966) The mineralogy of illites and mixed-layer illite-montmorillonites, Am.Miner, 825853.Google Scholar
Huff, W.D., Whiteman, J.H. & Curtis, C.D. (1988) Investigation of a K-bentonite by X-ray powder diffraction and analytical transmission electron microscopy. Clays Clay Miner., 3 , 8393.Google Scholar
Hughes, W.D., Whiteman, J.H. & Curtis, C.D. (1988) Investigation of a K-bentonite by X-ray powder diffraction and analytical transmission electron microscopy. Clays Clay Miner., 3 , 8393.Google Scholar
Hughes, C.R., Curtis, C.D., Whiteman, J.A., Heping, Sun, Whittle, C.K. & Ireland, B.J. (1990) Selected applications of analytical electron microscopy in clay mineralogy. Pp. 6988 in: CMS Workshop Lectures, vol., 2, Electron Optical Methods in Clay Science(I.D.R. Mackinnon & Mumpton, F. A., editors). The Clay Minerals Society, Evergreen, Colorado.Google Scholar
Inoue, A., Watanabe, T., Kohyama, N. & Brusewitz, A.M. (1990) Characterization of illitization of smectite in bentonite beds at Kinnekulle, Sweden. Clays Clay Miner., 38, 241–249.CrossRefGoogle Scholar
Ireland, B.J., Curtis, C.D. & Whiteman, J.A. (1983) Compositional variation within some glauconites and illites and implications for their stability and origins. Sedimentology, 30, 769–786.CrossRefGoogle Scholar
Kelley, W.P. (1945) Calculating formulas for fine grained minerals on the basis of chemical analysis. Am. Miner., 30, 1–26.Google Scholar
Klimentidis, R.E. & Mackinnon, I.D.R. (1986) High-resolution imaging of ordered mixed-layer clays. Clays Clay Miner., 34, 155–164.Google Scholar
Knipe, R.J. (1979) Chemical changes during slaty cleavage development. Bull Mineral., 02, 206–209.Google Scholar
Lee, J.H., Ahn, J.H. & Peacor, D.R. (1985) Textures in layered silicates: Progressive changes through diagenesis and low temperature metamorphism. J. Sed. Pet., 55, 532–540.Google Scholar
Merino, E. & Ransom, B. (1982) Free energies of formation of illite solid solutions and their compositional dependence. Geochim. Cosmochim. Acta, 30, 29–39.Google Scholar
Nadeau, P.H. & Bain, D.C. (1986) Compositions of some smectites and diagenetic illitic clays and implications for their origin. Clays Clay Miner., 34, 455464.CrossRefGoogle Scholar
Nadeau, P.H., Tait, J.M., McHardy, W.J. & Wilson, M.J., (1984) Interstratified XRD characteristics of physical mixtures of elementary day particles. Clay Miner., 9, 67–76.Google Scholar
Newman, A.C.D. & Brown, G. (1987) The chemical constitution of clays. Pp. 1-128 in: Chemistry of Clays and Clay Minerals(Newman, A.C.D., editor). Mineralogical Society, London.Google Scholar
Pawloski, G.A. (1985) Quantitative determination of mineral content of geological samples by X-ray diffraction. Am. Miner,, 70, 663–667.Google Scholar
Ransom, B. & Helgeson, H.C. (1989) On the correlation of expandability with mineralogy and layering in mixed- layer clays. Clays Clay Miner., 37, 189–191.CrossRefGoogle Scholar
Reynolds, R.C. (1990) Principles and techniques of quantitative analysis of clay minerals by X-ray powder diffraction. Pp. 438 in: CMS Workshop Lectures, vol. 1, Quantitative Mineral Analysis of Clays(Pevear, D.R. & Mumpton, F.A., editors). The Clay Minerals Society, Boulder, Colorado.Google Scholar
Ross, C.S. & Hendricks, S.B. (1945) Minerals of the montmorillonite group: Their origin and relation to soils and clays. U.S. Geol. Surv. Prof. Paper, 205-B, 2379.Google Scholar
Schultz, L.G. (1969) Lithium and potassium absorption, dehydroxylation temperature and structural water content of aluminous smectites. Clays Clay Miner., 9, 137–150.Google Scholar
Schwertmann, U. (1979) Non-crystalline and accessory minerals. Proc. 6th Jnt. Clay Conf., Oxford,, 491-499. Google Scholar
Scott, V.D. & Love, G. (1983) Quantitative Electron-Probe Microanalysis.Ellis Horwood, Chichester.Google Scholar
Shaw, H.F. & Primmer, T.J. (1989) Diagenesis in shales from a partly overpressured sequence in the Gulf Coast, Texas, USA. Mar. Petrol. Geol., 6, 121–128.Google Scholar
Środoń, J. (1980) Precise identification of illite/smectite interstratifications by X-ray powder diffraction. Clays Clay Miner., 28, 401411.CrossRefGoogle Scholar
Thorez, J. (1985) Qualitative clay mineral analysis biased by sample treatments. Proc. 5th Euroclay Meet, Prague,, 383389.Google Scholar
Till, R. & Spears, D.A. (1969) The determination of quartz in sedimentary rocks using an X-ray diffraction method. Clays Clay Miner., 17, 323–327.Google Scholar
Veblen, D.R., Guthrie, G.D., Livi, K.J.T. & Reynolds, R.C. (1990) High-resolution transmission electron microscopy and electron diffraction of mixed-layer illite/smectite: Experimental results. Clays Clay Miner., 38, 1–13.Google Scholar
Velde, B. (1977) A proposed phase diagram for illite, expanding chlorite, corrensite and illite-montmorillonite mixed layered minerals. Clays Clay Miner., 25, 264–270.Google Scholar
Velde, B. & Nicot E, (1985) Diagenetic clay mineral composition as a function of pressure, temperature, and chemical activity. J. Sed. Pet., 55, 541–547.Google Scholar
Warren, E.A. & Curtis, C.D. (1989) The chemical composition of authigenic illite within two sandstone reservoirs as analysed by ATEM. Clay Miner., 24, 137–156.Google Scholar
Weaver, C.E. & Pollard, L.D. (1973) The Chemistry of Clay Minerals. Elsevier, Amsterdam.Google Scholar
Weir, A.H. (1965) Potassium retention in clay minerals. Clay Miner., 6, 17–22.Google Scholar
Woodward, K. & Curtis, C.D. (1988) Predictive modelling of the distribution of production-constraining illites — Morecambe Gas Field, Irish Sea, offshore UK. Pp. 205-215 in: Petroleum Geology of North West Europe(Brooks, J. & Glennie, K., editors). Graham & Trotman, London.Google Scholar
Yau, Y.C., Peacor, D.R. & McDowell, S.D. (1987) Smectite-to-illite reactions in Salton Sea shales: A transmission and analytical electron microscopy study, J. Sed. Pet., 57, 335–342.Google Scholar