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Change in Layer Charge of Smectites and Smectite Layers in Illite/Smectite During Diagenetic Alteration

Published online by Cambridge University Press:  28 February 2024

Tsutomu Sato ,
Takashi Murakami  and
Takashi Watanabe
Tsutomu Sato
Affiliation:
Department of Environmental Safety Research, Japan Atomic Energy Research Institute, Tokai, Ibaraki 319-11, Japan
Takashi Murakami*
Affiliation:
Department of Earth Sciences, Ehime University, Matsuyama, Ehime 790, Japan
Takashi Watanabe
Affiliation:
Department of Geoscience, Joetsu University of Education, Yamayashiki, Joetsu, Niigata 943, Japan
*
†Present address: Mineralogical Institute, Graduate School of Science, The University of Tokyo, Hongo Bunkyo-ku, Tokyo 113, Japan.
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Abstract

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The changes in amount and location of layer charge during diagenetic alteration have been investigated for smectites and smectite layers of illite/smectite interstratified minerals (I/S) by X-ray powder diffraction analysis with various expansion behavior tests: 1) ethylene glycol (EG) solvation (XRD); 2) K-saturation and EG solvation; 3) Li-saturation, heating at 250 °C and glycerol or EG solvation (Greene-Kelly test); and 4) alkylammonium saturation. In the course of low-temperature diagenesis but before the onset of illitization, mean layer charge of smectites continuously increases from approximately 0.56 to 0.73 per O20(OH)4 with increasing depth, and tetrahedral charge also increases continuously from approximately 0.21 to 0.38 per O20(OH)4 (beidellitization). The continuous increase in tetrahedral charge without change in peak intensity and shape suggests that the solid-state Al for Si substitution mechanism appears to predominate within beidellitization. After illitization, the content of the beidellitic layers continuously decreases, while the mean layer charge of expandable layers and the content of illite layers in I/S increase. This suggests that the conversion of a beidellitic layer to an illitic layer preferably occurs during early illitization. Thus, before illitization, beidellite-like layers are formed from precursor smectite, and during the early stage of illitization, the high charged beidellitic layers are probably consumed to form illite layers.

Keywords

BeidellitizationCharge LocationDiagenesisGreene-Kelly TestMite/SmectiteLayer ChargeSmectite
Type
Research Article
Information
Clays and Clay Minerals , Volume 44 , Issue 4 , August 1996 , pp. 460 - 469
Copyright
Copyright © 1996, The Clay Minerals Society

References

Bethke, G.M. and Altaner, S.P.. 1986. Layer-by-layer mechanism of smectite illitization and application to a new rate law. Clays & Clay Miner 34: 136–145.CrossRefGoogle Scholar
Bethke, G.M., Vergo, N. and Altaner, S.P.. 1986. Pathways of smectite illitization. Clays & Clay Miner 34: 125–135.CrossRefGoogle Scholar
Boles, J.R. and Franks, S.G.. 1979. Clay diagenesis in Wilcox sandstones of southwest Texas: Implications of smectite diagenesis on sandstone cementation. J Sed Petrol 49: 55–70.Google Scholar
Brindley, G.W.. 1966. Ethylene glycol and glycerol complexes of smectites and vermiculites. Clay Miner 6: 237–259.CrossRefGoogle Scholar
Bruce, C.H.. 1984. Smectite dehydration—Its relation to structural development and hydrocarbon accumulation in northern Gulf of Mexico basin. Am Assoc Petrol Geol Bull 68: 637–683.Google Scholar
Brusewitz, A.M.B.. 1986. Chemical and physical properties of Paleozoic potassium bentonites from Kinnekulle, Sweden. Clays & Clay Miner 34: 442–454.CrossRefGoogle Scholar
Burst, J.F.. 1969. Diagenesis of Gulf Coast clayey sediments and its possible relation to petroleum migration. Am Assoc Petrol Geol Bull 53: 73–93.Google Scholar
Byström-Brusewitz, A.M.. 1975. Studies on the Li test to distinguish between beidellite and montmorillonite. Proc Intern Clay Conf, 1972, Mexico City. Wilmette, IL: Applied Publishing Ltd. p 419–428.Google Scholar
Calvet, R. and Prost, R.. 1971. Cation migration into empty octahedral sites and surface properties of clays. Clays & Clay Miner 19: 175–186.CrossRefGoogle Scholar
Cetin, K. and Huff, W.D.. 1995. Layer charge of the expandable component of illite/smectite in K-bentonite as determined by alkylammonium ion exchange. Clays & Clay Miner 43: 150–158.CrossRefGoogle Scholar
Christidis, G. and Dunham, A.C.. 1993. Compositional variations in smectites. 1. Alteration of intermediate volcanic rocks—A case study from Milos-island, Greece. Clay Miner 28: 255–273.CrossRefGoogle Scholar
Eberl, D.D.. 1978. Reaction series for dioctahedral smectites. Clays & Clay Miner 26: 327–340.CrossRefGoogle Scholar
Eberl, D.D.. 1993. Three zones for illite formation during burial diagenesis and metamorphism. Clays & Clay Miner 41: 26–37.CrossRefGoogle Scholar
Eberl, D.D. and Srodon, J.. 1988. Ostwald ripening and interparticle-diffraction effects for illite crystals. Am Miner 73: 1335–1345.Google Scholar
Eberl, D.D., Srodon, J., Kralik, M., Taylor, B.E. and Peterman, Z.E.. 1990. Ostwald ripening of clays and metamorphic minerals. Science 248: 474–477.CrossRefGoogle Scholar
Eberl, D.D., Srodon, J. and Northrop, H.R.. 1986. Potassium fixation in smectite by wetting and drying. In: Davis, J.A. and editors, Hayes. Geochemical processes at mineral surfaces. Washington, DC: Am Chem Soc p 296–326.Google Scholar
Eslinger, E., Highsmith, P., Albers, D. and DeMayo, B.. 1979. Role of iron reduction in the conversion of smectite to illite in bentonites in the disturbed belt, Montana. Clays & Clay Miner 27: 327–338.CrossRefGoogle Scholar
Glaeser, R. and Mering, J.. 1968. Homogeneous hydration domains of the smectite. CR Hebd Seanc Acad Sci, Paris 46: 436–466.Google Scholar
Greene-Kelly, R.. 1953. Irreversible dehydration in montmorillonite. Part II Clay Miner Bull 2: 52–56.CrossRefGoogle Scholar
Greene-Kelly, R.. 1955. Dehydration of montmorillonite minerals. Miner Mag 30: 604–615.Google Scholar
Harward, M.E. and Brindley, G.W.. 1965. Swelling properties of synthetic smectite in relation to lattice substitutions. Clays & Clay Miner 13: 209–222.CrossRefGoogle Scholar
Hausler, W. and Stanjek, H.. 1988. A refined procedure for the determination of the layer charge with alkylammonium ions. Clay Miner 23: 333–337.CrossRefGoogle Scholar
Hofmann, U. and Klemen, R.. 1950. Verlust der austauschfahigkeit von lithiumionen an bentonit durch erhitzung. Z Anorg Chem 262: 95–99.CrossRefGoogle Scholar
Howard, J.J.. 1981. Lithium and potassium saturation of illite/smectite clays from interlaminated shales and sandstones. Clays & Clay Miner 29: 136–142.CrossRefGoogle Scholar
Howard, J.J. and Roy, D.M.. 1985. Development of layer charge and kinetics of experimental smectite alteration. Clays & Clay Miner 33: 81–88.CrossRefGoogle Scholar
Hower, J., Eslinger, E.V., Hower, M.E. and Perry, E.A.. 1976. Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence. Bull Geol Soc Am 87: 725–735.2.0.CO;2>CrossRefGoogle Scholar
Hower, J. and Mowatt, T.C.. 1966. The mineralogy of illites and mixed-layer illite/montmorillonites. Am Mineral 51: 825–854.Google Scholar
Inoue, A., Minato, H. and Utada, M.. 1978. Mineralogical properties and occurence of illite/montmorillonite mixed layer minerals formed from miocene volcanic glass in Waga-Omono district. Clay Sci 5: 123–136.Google Scholar
Inoue, A. and Utada, M.. 1983. Further investigations of a conversion series of dioctahedral mica/smectites in the Shinzan hydrothermal alteration area, northeast Japan. Clays & Clay Miner 31: 401–412.CrossRefGoogle Scholar
Inoue, A., Velde, B., Meunier, A. and Touchard, G.. 1988. Mechanism of illite formation during smectite-to-illite conversion in a hydrothermal system. Am Mineral 73: 1325–1334.Google Scholar
Kodama, H. and Ross, G.J.. 1974. Effect of layer charge location on potassium exchange and hydration of mica. Am Mineral 59: 491–495.Google Scholar
Lagaly, G., Fernandez-Gonzalez, M. and Weiss, A.. 1976. Problems in layer-charge determination of montmorillonites. Clay Miner 11: 173–187.CrossRefGoogle Scholar
Lagaly, G. and Weiss, A.. 1969. Determination of the layer charge in mica-type layer silicates. Proc Int Clay Conf, Tokyo, 1969. p 173–187.Google Scholar
Lanson, B. and Champion, D.. 1991. The I/S- to illite reaction in the late stage diagenesis. Am J Sci 291: 473–506.CrossRefGoogle Scholar
Machajdik, D. and Cicel, B.. 1981. Potassium- and Ammonium-treated montmorillonites. II. Calculation of characteristic layer charge. Clays & Clay Miner 29: 47–52.CrossRefGoogle Scholar
Malla, P.B. and Douglas, L.A.. 1987a. Identification of expanding layer silicates: Layer charge vs. expansion properties. Proc Internat Clay Conf p 277–283.Google Scholar
Malla, P.B. and Douglas, L.A.. 1987b. Layer charge properties of smectites and vermiculites: Tetrahedral vs. octahedral. Soil Sci Soc Am J 51: 1362–1366.CrossRefGoogle Scholar
Malla, P.B. and Douglas, L.A.. 1987c. Problems in identification of montmorillonite and beidellite. Clays & Clay Miner 35: 232–236.CrossRefGoogle Scholar
McDowell, S.D. and Elders, W.A.. 1980. Authigenic layer silicate minerals in borehole Elmore 1, Saltan Sea geothermal field, California, U.S.A.. Contrib Mineral Petrol 74: 293–310.CrossRefGoogle Scholar
Meunier, A. and Velde, B.. 1989. Solid solutions in I/S mixed-layer minerals and illite. Am Mineral 74: 1106–1112.Google Scholar
Nadeau, P.H. and Bain, D.C.. 1986. Composition of some smectites and diagenetic illitic clays and implications for their origin. Clays & Clay Miner 34: 455–464.CrossRefGoogle Scholar
Nadeau, P.H. and Reynolds, R.C.. 1981. Burial and contact metamorphism in the Mancos shale. Clays & Clay Miner 29: 249–259.CrossRefGoogle Scholar
Nadeau, P.H., Wilson, M.J., McHardy, W.J. and Tait, J.M.. 1985a. The conversion of smectite to illite during diagenesis: Evidence from some illitic clays from bentonites and sandstones. Miner Mag 49: 393–400.CrossRefGoogle Scholar
Nadeau, P.H., Farmer, V.C., McHardy, W.J. and Bain, D.C.. 1985b. Compositional variations of the Unterrupsroth beidellite. Am Mineral 70: 1004–1010.Google Scholar
Nishida, S., Tsuda, K. and Ichimura, R.. 1966. On the Neogene deposits of the northern part of the Fossa Magna region.— Studies of the so-called “Nambayama Formation” Part I-. Sci Rep Niigata Univ 1: 15–20 (in Japanese).Google Scholar
Olis, A.C., Malla, P.B. and Douglas, L.A.. 1990. The rapid estimation of the layer charges of 2: 1 expanding clays from a single alkylammonium ion expansion. Clay Miner 25: 39–50.CrossRefGoogle Scholar
Perry, E. and Hower, J.. 1970. Burial diagenesis in Gulf Coast pelitic sediments. Clays & Clay Miner 18: 165–177.CrossRefGoogle Scholar
Reynolds, R.C. and Hower, J.. 1970. The nature of interlayering in mixed-layer illite-montmorillonites. Clays & Clay Miner 18: 25–36.CrossRefGoogle Scholar
Sato, T. and Watanabe, T.. 1989. Diagenetic alteration of Neogene sedimentary rocks in the No district, Niigata Prefecture. J Jpn Assoc Miner Petrol Econ Geol 84: 259–269 (in Japanese).CrossRefGoogle Scholar
Sato, T., Watanabe, T. and Otsuka, R.. 1992. Effects of layer charge, charge location, and energy change on expansion properties of dioctahedral smectites. Clays & Clay Miner 40: 103–113.CrossRefGoogle Scholar
Srodon, J., Elsass, F., McHardy, W.J. and Morgan, D.J.. 1992. Chemistry of illite-smectite inferred from TEM measurements of fundamental particles. Clay Miner 27: 137–158.CrossRefGoogle Scholar
Srodon, J., Morgan, D.J., Eslinger, E.V., Eberl, D.D. and Karlinger, M.R.. 1986. Chemistry of illite/smectite and end-member illite. Clays & Clay Miner 34: 368–378.CrossRefGoogle Scholar
Stanjek, H. and Friedrich, R.. 1986. The determination of layer charge by curve-fitting of Lorentz- and polarization-corrected X-ray diagrams. Clay Miner 21: 183–190.CrossRefGoogle Scholar
Steiner, A.. 1968. Clay minerals in hydrothermally altered rocks at Wairakei, New-Zealand. Clays & Clay Miner 16: 193–213.CrossRefGoogle Scholar
Stul, M.S. and Mortier, W.J.. 1974. The heterogeneity of the charge density in montmorillonites. Clays & Clay Miner 22: 391–396.CrossRefGoogle Scholar
Suquet, H., De La Calle, C. and Pezerat, H.. 1975. Swelling and structural organization of saponite. Clays & Clay Miner 23: 1–9.CrossRefGoogle Scholar
Suquet, H., Iiyama, J.T., Kodama, H. and Pezerat, H.. 1977. Synthesis and swelling properties of saponites with increasing layer charge. Clays & Clay Miner 25: 231–242.CrossRefGoogle Scholar
Velde, B. and Brusewitz, A.M.. 1982. Metasomatic and nonmeta-somatic low grade metamorphism of Ordovician meta-bentonites in Sweden. Geochim Cosmochim Acta 46: 447–452.CrossRefGoogle Scholar
Velde, B. and Brusewitz, A.M.. 1986. Compositional variation in component layers in natural illite/smectite. Clays & Clay Miner 34: 651–657.CrossRefGoogle Scholar
Watanabe, T.. 1988. The structural model of illite/smectite interstratified mineral and the diagram for its identification. Clay Sci 7: 97–114.Google Scholar
Whitney, G.. 1992. Dioctahedral smectite reactions at elevated temperatures: Effects of K-availability, Na/K ratio and ionic strength. Appl Clay Sci 7: 97–112.CrossRefGoogle Scholar
Whitney, G. and Northrop, R.. 1988. Experimental investigation of the smectite to illite reaction: Dual reaction mechanisms and oxygen-isotope systematics. Am Mineral 73: 77–90.Google Scholar
Whitney, G. and Velde, B.. 1993. Changes in particle morphology during illitization—An experimental study. Clays & Clay Miner 41: 209–218.CrossRefGoogle Scholar