Abstract
Iron oxides have long been recognised by different disciplinary groups to be important constituents of most soils. This group of minerals (which includes the oxy-hydroxides and the hydrous oxides) influences such diverse properties as, for example, fertility, structure, permeability, soil colour, and profile differentiation. They can exercise a role in microbial respiration, and they can act as a sink and/or source of potentially toxic heavy metal pollutants. These minerals seem to be examined and categorised by each new analytical tool developed, and new techniques are constantly being tried to describe more precisely the concentrations of the different phases present, their inter-relationships, their compositions, and variabilities.
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References
Bernal, J.O., Dasgupta, D.R. and Mackay, A.L. 1959. The oxides and hydroxides of iron and their structural inter-relationships. Clay Min. Bull. 4, 15–30.
Cromer, R.N. and Vines, R.G. 1966. Soil temperatures under a burning windrow. Aust. For. Res. 2, 29–34.
Detournay, J., Ghodsi, M. and Derie, R. 1975. Influence de la température et de la présence des ions étrangers sur la cenétique et le mécanisme de formation de la goethite en milieu aqueux. Z. anorg. allg. chem. 412, 184–192.
Fauck, R. 1974. Les facteurs et les mécanismes de la pédogenese dans les sols rouges et jaunes sur sable et grés en Afrique. Cah. O.R.S.T.O.M. Ser. Pedol. 12, 69-72.
Fischer, W.R. and Schwertmann, U. 1975. The formation of hematite from amorphous iron (III)-hydroxide. Clays Clay Miner. 23, 33–37.
Fitzpatrick, R.W. 1978. Occurrence and properties of Fe and Ti oxides in soils along Eastern seaboard of South Africa. Ph.D. Thesis. University of Natal, Pietermaritzburg.
Fitzpatrick, R.W. 1983. Effect of forest and grass burning on mineralogical transformations in some soils of Natal. Soils & Irrigation Research Institute. Report No. 952/139/80.
Gastuche, M.C., Bruggenwert, T. and Mortland, M.M. 1964. Crystallisation of mixed iron and aluminium gels. Soil Sci. 98, 281–289.
Krause, A. and Borkowska, A. 1963. Der Einfluß von Fremdanionen auf die Luftoxydation von Fe(OH)2 and die Struktur der Oxydations-produkte. Z. anorg. allg. Chem. 326, 216–224.
Kodama, H. and Schnitzer, M. 1977. Effect of fulvic acid on the crystallisation of Fe(III) oxides. Geoderma 19, 279–291.
Le Borgne, E. 1955. Abnormal magnetic susceptibility of the top soil. Annls. Geophys. 11, 399–419.
Lieser, K.H. and Schroeder, H. 1959. Kinetics of solution of anhydrous Fe(III) sulphate in solutions containing Fe(II) ions. Z. Electrochem. 64, 252–257.
McHardy, W.J. (the late), Thompson, A.P. and Goodman, B.A. 1974. Formation of iron oxides by decomposition of iron-phenolic chelates. J. Soil Sci. 25, 471–482.
McKenzie, R.M. 1980. The adsorption of lead and other heavy metals on oxides of manganese and iron. Aust. J. Soil Res. 18, 61–73.
Milnes, A.R., Bourman, R.P. and Fitzpatrick, R.W. 1985. Petrology and minerology of ‘laterites’ in southern and eastern Australia. Proc. Intern. Seminar on Laterite, Tokyo, Oct. 1985 Vol. A, 163–178.
Murad, E. and Taylor, R.M. 1984. The Mössbauer spectra of hydroxycarbonate green rusts. Clay Min. 19, 77–83.
Nalovic, L. 1974. Geochemical research on transition elements in soils. An experimental study of the influence of trace elements on the behaviour of iron and the evolution of ferriferous compounds during pedogenesis. Summary of Thesis for ‘Doctorat d’Etat’ Paris University VI.
Nalovic, L.J., Pedro, G. and Janot, C. 1975. Demonstration by Mössbauer spectroscopy of the role played by transitional trace elements in the crystallogenesis of iron hydroxides (III). Proc. Intern. Clay Conf., Mexico City, pp. 601-610.
Norrish, K. and Taylor, R.M 1961. The isomorphous replacement of iron by aluminium in soil goethites. J. Soil Sci. 12, 294–306.
Oades, J.M. and Townsend, W.N. 1963. The detection of ferromagnetic minerals in soils and clays. J. Soil Sci. 14, 179–87.
Rowell, D.L. 1981. Oxidation and reduction. In D.J. Greenland and M.H.B. Hayes (eds.), The Chemistry of Soil Processes. Wiley, Chichester, pp. 401–461.
Schellmann, W. 1959. Experimentelle Untersuchungen über die sedimentäre Bildung von Goethite und Hämatit. Chem. Erde 20, 104–35.
Schwertmann, U. 1959a. Über die Sythese definierter Eisenoxyde unter verschiedenen Bedingungen. Z. anorg. allg. Chem. 298, 337–48.
Schwertmann, U., Fitzpatrick, R.W., Taylor, R.M. and Lewis, D.G. 1979. The influence of aluminium on iron oxides. Part II. Preparation and properties of Al substituted hematites. Clays Clay Min. 27, 105–112.
Schwertmann, U. and Heinemann, B. 1959. Über das Vorkommen und die Enstehung von Maghemit in nordwestdeutschen Böden. Neves Jahrb.-Minerals. Monatsh. 174-181.
Schwertmann, U. and Taylor, R.M. 1972. The transformation of lepidocrocite to goethite. Clays Clay Miner. 20, 151–158.
Schwertmann, U. and Taylor, R.M. 1972b. The influence of silicate on the transformations of lepidocrocite to goethite. Clays Clay Miner. 20, 159–164.
Schwertmann, U. and Taylor, R.M. 1977. Iron oxides. In J.B. Dixon and S.B. Weed (eds.), Minerals in Soil Environments. Soil Sci. Soc. Amer. Inc., Wisconsin, pp. 145–180.
Schwertmann, U. and Taylor, R.M. 1979. Natural and synthetic poorly crystallised lepidocrocite. Clay Miner. 14, 285–293.
Schwertmann, U. and Thalman, H. 1976. The influence of [Fe(II)], [Si] and pH on the formation of lepidocrocite and ferrihydrite during oxidation of aqueous FeCL2 solutions. Clay Min. 11, 189–200.
Tamaura, Y., Ito, K. and Katsura, T. 1983. Transformation of γ-FeO(OH) to Fe3O4 by adsorption of Iron(II) ion on γ-FeO(OH). J. Chem. Soc. Dalton Trans. 189-194.
Taylor, R.M 1980. Formation and properties of Fe(II)Fe(III) hydroxy-carbonate and its possible significance in soil formation. Clay Min. 15, 369–382.
Taylor, R.M 1984a. The influence of chloride on the mineralisation of Fe from the Fe(II) system. I. Effects of Cl on the formation of magnetite. Clays Clay Min. 32, 167–184.
Taylor, R.M. 1984b. Rapid formation of crystalline double hydroxy salts. Clay Min. 19, 591–603.
Taylor, R.M. and McKenzie, R.M. 1980. The influence of Al on iron oxides. Part VI. The formation of Fe(II)-Al(III) hydroxy-chlorides,-sulphates, and-carbonates as new members of the pyroaurite group and their possible significance in soils. Clays Clay Min. 28, 179–187.
Taylor, R.M. and Schwertmann, U. 1974. Maghemite in soils and its origin. 1. Properties and observations on soil maghemites. Clay Minerals 10, 289–298.
Taylor, R.M. and Schwertmann, U. 1978. The influence of Al on iron oxides. 1. The influence of Al on Fe oxide formation from the Fe(II) system. Clays Clay Min. 26, 373–383.
Taylor, R.M., Self, P.G. and Fitzpatrick, R.W. 1986. The influence of sucrose and glycerol on the formation and transformations of iron oxide — the implication for soil formation. Appl. Clay Sci. (in press).
Towe, K.W. and Bradley, W.F. 1967. Mineralogical constitution of colloidal hydrous ferric oxides. J. Colloid Interface Sci. 24, 384–392.
van der Marel, H.W. 1951. Gamma ferric oxide in sediments. J. Sediment. Petrol. 21, 12–21.
Vodyanitskii, Yu. N. 1981. Formation of ferromagnetic minerals in soil — podzolic soils. Pochvovedenie 5, 114–123.
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Taylor, R.M. (1990). Some Observations on the Formation and Transformation of Iron Oxides. In: De Boodt, M.F., Hayes, M.H.B., Herbillon, A., De Strooper, E.B.A., Tuck, J.J. (eds) Soil Colloids and Their Associations in Aggregates. NATO ASI Series, vol 214. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-2611-1_4
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