Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-27T17:03:09.487Z Has data issue: false hasContentIssue false

Synthetic Allophane and Layer-Silicate Formation in SiO2-Al2O3-FeO-Fe2O3-MgO-H2O Systems at 23°C and 89°C in a Calcareous Environment

Published online by Cambridge University Press:  02 April 2024

V. C. Farmer
Affiliation:
The Macaulay Land Use Research Institute, Aberdeen AB9 2QJ, United Kingdom
G. S. R. Krishnamurti
Affiliation:
Department of Soil Science, University of Saskatchewan, Saskatoon, Saskatchewan S7N 0W0, Canada
P. M. Huang
Affiliation:
Department of Soil Science, University of Saskatchewan, Saskatoon, Saskatchewan S7N 0W0, Canada
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.

Solutions containing AlCl3 and Si(OH)4 (concentrations ≤ 1.5 mM with molar Si:Al ratios of 1:2, 1:1 and 3:1) and FeCl2 (0, 0.5 and 1.0 mM) were adjusted to pH 8 with Ca(OH)2, and incubated at 23°C and 89°C without exclusion of air in the presence of CaCO3 for 8–12 weeks. The products were characterized by infrared spectroscopy and X-ray diffraction. Systems with 3:1 and 1:1 Si:Al ratios without Fe gave hydrous feldspathoids at 23° and 89°C. Systems with 3:1 Si:Al ratios containing Fe gave aluminous nontronites at 89°C and noncrystalline, nontronite-like products at 23°C. Systems with 1:1 Si:Al ratios with added Fe gave Fe(III)-substituted hydrous feldspathoids at 23°C. At 89°C, the system with 1:1 Si:Al ratios and 0.5 mM Fe produced a “protohalloysite,” while that with 1.0 mM Fe gave a poorly ordered nontronite-like layer silicate. In systems with 1:2 Si:Al ratios, the formation of “protoimogolite” at 23°C was little affected by additions of Fe. At 89°C, the “protoimogolite” decomposed to boehmite and poorly-ordered layer silicate phases. Inclusion of 1 mM MgCl2 in the above systems had no effect on the products at 23°C, but at 89°C produced saponites and a mixed layer saponite-chlorite in the 3:1 Si:Al systems, and saponite-like layer structures in the 1:1 and 1:2 Si:Al systems.

Type
Research Article
Copyright
Copyright © 1991, The Clay Minerals Society

References

Baes, C. F. and Mesmer, R. E., 1976 The Hydrolysis of Cations New York John Wiley & Sons.Google Scholar
Brindley, G. W., Brindley, G. W. and Brown, G., 1980 Order-disorder in clay mineral structures Crystal Structures of Clay Minerals and Their X-ray Identification London Mineralogical Society.CrossRefGoogle Scholar
Decarreau, A., 1981 Crystallogenèse à basse température de smectites trioctahedriques par vieillessement de copré-cipités silicometallique Compt. Rend. Sci. Paris, Ser. II 292 6164.Google Scholar
Decarreau, A. and Bonnin, D., 1986 Synthesis and crystallogenesis at low temperature of Fe(III) smectites by evolution of coprecipitated gels. Experiments in partially reducing conditions Clay Miner. 21 861867.CrossRefGoogle Scholar
Dougan, W. K. and Wilson, A. L., 1974 Absorptiometric determination of aluminum in water. Comparison of some chromogenic reagents and the development of an improved method Analyst (London) 99 413430.CrossRefGoogle ScholarPubMed
Duchaufour, P., 1982 Pedology: Pedogenesis and Classification London Allen & Unwin.CrossRefGoogle Scholar
Farmer, V. C., Fraser, A. R. and Tait, J. M., 1979 Characterization of the chemical structures of natural and synthetic aluminosilicate gels and sols by infrared spectrometry Geochim. Cosmochim. Acta 43 14171420.CrossRefGoogle Scholar
Farmer, V. C., McHardy, W. J., Palmieri, F., Violante, A. and Violante, P., 1991 Synthetic allophanes formed in calcareous environments. Nature, conditions of formation, and transformations Soil Sci. Soc. Am. J. .CrossRefGoogle Scholar
Goodman, B. A., Russell, J. D. and Fraser, A. R., 1976 A Mössbauer and IR spectroscopic study of the structure of nontronite Clays & Clay Minerals 24 5359.CrossRefGoogle Scholar
Harder, H., 1976 Nontronite synthesis at low temperature Chem. Geol. 18 169180.CrossRefGoogle Scholar
Krishnamurti, G. S. R. Huang, P. M., Farmer, V. C. and Tardy, Y., 1991 Kinetics of Fe(II) oxygenation and the nature of hydrolytic products as influenced by ligands Proc. 9th Int. Clay Conf. (Strasbourg, France) .Google Scholar
McBride, M. B., Farmer, V. C., Russell, J. D., Tait, J. M. and Goodman, B. A., 1984 Iron substitution in aluminosilicate sols synthesized at low pH Clay Miner. 19 18.CrossRefGoogle Scholar
Morrison, I. R. and Wilson, A. L., 1963 The absorptimetric determination of silicon in water, Part II Analyst (London) 88 100104.CrossRefGoogle Scholar
Parfitt, R. L. and Kimble, J. M., 1989 Conditions for formation of allophanes in soils Soil Sci. Soc. Am. J. 53 971977.CrossRefGoogle Scholar
Russell, J. D. and Wilson, M. J., 1987 Infrared methods A Handbook of Determinative Methods in Clay Mineralogy New York Blackie, Glasgow and Chapman and Hall 133173.Google Scholar
Shayan, A., 1984 Hisingerite material from a basalt quarry near Geelong, Victoria, Australia Clays & Clay Minerals 32 272278.CrossRefGoogle Scholar
Wada, K., Wilson, M., Kakuto, Y. and Wada, S.-I., 1988 Synthesis and characterization of a hollow spherical form of monolayer aluminosilicate Clays & Clay Minerals 36 1118.CrossRefGoogle Scholar
Whelan, J. A. and Goldich, S. S., 1961 New data for hisingerite and neotocite Amer. Mineral. 46 14121423.Google Scholar
Wilson, M. J. and Wilson, M.J., 1987 X-ray powder diffraction methods A Handbook of Determinative Methods in Clay Mineralogy New York Blackie, Glasgow and Chapman and Hall 2698.Google Scholar