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Fuzzy Phase Diagrams of Clay Minerals

Published online by Cambridge University Press:  01 January 2024

Chandrika Varadachari*
Affiliation:
Raman Centre for Applied and Interdisciplinary Sciences, 16A Jheel Road, Calcutta 700 075, India
*
*E-mail address of corresponding author: RCAIS@CAL3.VSNL.NET.IN

Abstract

This paper presents a novel concept in the thermodynamic derivation of phase diagrams for clay minerals that incorporates fuzzy transition zones. This new technique yields phase diagrams that have graded (fuzzy) zones of mineral occurrences and includes compositional variability within mineral groups. For the construction of these diagrams, 170 minerals belonging to nine different subgroups were used, based on a fuzzy mathematical description of their ‘grades’ or ‘belonging-ness’. Standard free energies of formation of all the minerals were derived and all possible pairs of mineral equilibria were evaluated. Relative intensities of mineral occurrences were determined and membership values of each type of mineral at various zones in a 2D or 3D space were graphically represented. Computations and graphical representations were carried out using programs developed in Mathematica. Diagrams were derived for 25°C, 1 bar with a solution phase containing Si(OH)4, K+, Na+, H+, Ca2+ and Mg2+ under conditions of gibbsite, goethite and ferrous oxide saturation. The resulting diagrams, unlike conventional phase diagrams, show multimineral assemblages, with varying occurrences of different minerals and provide a realistic representation of clay mineral occurrences formed by surface geochemical processes. They show that on the Earth’s surface, only montmorillonite can almost completely predominate the inorganic phase followed by kaolinite, illite and beidellite. Nontronite, glauconite, celadonite and vermiculite would not be neoformed in substantial amounts. A general conformity of derived phase equilibria with experimentally observed equilibria is also observed.

Type
Research Article
Copyright
Copyright © 2006, The Clay Minerals Society

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References

Aja, S.U. Rosenberg, P.E. and Kittrick, J.A., (1991) Illite equilibria in solutions: I. Phase relationships in the system K2O-Al2O3-SiO2-H2O between 25 and 250°C Geochimica et Cosmochimica Acta 55 13531364 10.1016/0016-7037(91)90313-T.CrossRefGoogle Scholar
Garrels, R.M. and Christ, C.L., (1965) Solutions, Minerals and Equilibria New York Harper & Row.Google Scholar
Helgeson, H.C. Brown, T.H. and Leeper, R.H., (1969) Handbook of Theoretical Activity Diagrams Depicting Chemical Equilibria in Geologic Systems Involving an Aqueous Phase at One Atm and 0° to 300°C Cooper & Company, San Francisco Freeman.Google Scholar
Johnson, J.W. Oelkers, E.H. and Helgeson, H.C., (1992) SUPCRT92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5000 bars and 0 to 1000°C Computers and Geosciences 18 899947 10.1016/0098-3004(92)90029-Q.CrossRefGoogle Scholar
Klir, G. and Yuan, B., (1997) Fuzzy Sets and Fuzzy Logic New Delhi Prentice-Hall.Google Scholar
Kudrat, M. Sharma, K.P. Varadachari, C. and Ghosh, K., (1999) An algorithm and program in C-language for computation of standard free energy of formation of clay minerals Computers and Geosciences 25 241250 10.1016/S0098-3004(98)00170-8.CrossRefGoogle Scholar
Kudrat, M. Varadachari, C. and Ghosh, K., (2000) Application of the improved regression method to derive ΔGf0 of non-stoichiometric clay minerals and their correlations with compositional parameters Chemical Geology 168 225238 10.1016/S0009-2541(00)00196-0.CrossRefGoogle Scholar
Norton, D., (1974) Chemical mass transfer in the Rio Tanama system, west-central Puerto Rico Geochimica et Cosmochimica Acta 38 267277 10.1016/0016-7037(74)90110-0.CrossRefGoogle Scholar
Robie, R.A. Hemingway, B.S. and Fisher, J.R., (1978) Thermodynamic properties of minerals and related substances at 298.15°K and 1 bar (105 pascals) pressure and at higher temperature US Geological Survey Bulletin 1452 1456.Google Scholar
Tardy, Y., (1971) Characterisation of the principal weathering types by the geochemistry of waters from some European and African crystalline massifs Chemical Geology 7 253271 10.1016/0009-2541(71)90011-8.CrossRefGoogle Scholar
Tardy, Y. Duplay, J., Wolf, K.H. and Chilingarian, G.V., (1994) Stability fields of smectites and illites including glauconites as a function of temperature and chemical composition Diagenesis IV Amsterdam Elsevier 95132 10.1016/S0070-4571(08)70438-2.CrossRefGoogle Scholar
Varadachari, C., (1992) Constructing phase diagrams for silicate minerals in equilibrium with an aqueous phase: A theoretical approach Soil Science 153 512 10.1097/00010694-199201000-00002.CrossRefGoogle Scholar
Varadachari, C. and Ghosh, K., (2003) Thermodynamic derivation of new low temperature phase diagrams for phyllosilicates defining stable and metastable phases Indian Journal of Geology 75 203217.Google Scholar
Varadachari, C. and Mukherjee, G., (2004) Discriminant analysis of clay mineral compositions Clays and Clay Minerals 52 311320 10.1346/CCMN.2004.0520306.CrossRefGoogle Scholar
Varadachari, C. Kudrat, M. and Ghosh, K., (1994) Evaluation of standard free energies of formation of clay minerals by an improved regression method Clays and Clay Minerals 42 298307 10.1346/CCMN.1994.0420308.CrossRefGoogle Scholar
Varadachari, C. Mukherjee, G. Goswami, D.P. and Chakraborty, M.K., (2003) Understanding clay minerals with fuzzy mathematics Naturwissenschaften 90 4448.CrossRefGoogle ScholarPubMed