Hostname: page-component-7dd5485656-glrdx Total loading time: 0 Render date: 2025-10-31T03:34:11.478Z Has data issue: false hasContentIssue false
  • English
  • Français

Nature and origin of an aluminous vermiculitic weathering product in acid soils from upland catchments in Scotland

Published online by Cambridge University Press:  09 July 2018

D. C. Bain ,
A. Mellor  and
M. J. Wilson
D. C. Bain
Affiliation:
The Macaulay Land Use Research Institute, Craigiebuckler, Aberdeen AB9 2QJ, Scotland
A. Mellor
Affiliation:
The Macaulay Land Use Research Institute, Craigiebuckler, Aberdeen AB9 2QJ, Scotland
M. J. Wilson
Affiliation:
The Macaulay Land Use Research Institute, Craigiebuckler, Aberdeen AB9 2QJ, Scotland
Get access Rights & Permissions [Opens in a new window]

Abstract

Vermiculitization of mica is one of the main weathering processes in soils from three upland catchments receiving various levels of acid deposition. Usually this process is manifested by the presence of interstratified mica-vermiculite with the interlayer space in the vermiculite often partially filled with polymeric hydroxyaluminium species. In one peaty podzol, regularly interstratified mica-vermiculite clearly develops at the expense of mica and is the dominant mineral in the Eh horizon. It was concentrated by chemical treatments to remove organic matter, free iron oxides, and any Al species in the interlayer, and the structural formula calculated from chemical analysis confirmed the dioctahedral character of both vermiculite and mica components, and indicated that the vermiculitic weathering product was formed from a dioctahedral mica. The degree of interlayering in the interstratified phases seemed to be pH-dependent with resultant implications for soil and freshwater acidification.

Information

Type
Research Article
Information
Clay Minerals , Volume 25 , Issue 4 , December 1990 , pp. 467 - 475
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1990

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.)

Article purchase

Temporarily unavailable

References

April, R.H., Hluchy, M.M. & Newton, R.M. (1986) The nature of vermiculite in Adirondack soils and till. Clays Clay Miner., 34, 549–556.CrossRefGoogle Scholar
Barnhisel, R.I. & Bertsch, P.M. (1989) Chlorites and hydroxy-interlayered vermiculite and smectite. Pp. 729–788 in: Minerals in Soil Environments (J.B. Dixon & S.B. Weed, editors). Soil Sci. Soc. Am., Madison, Wisconsin.Google Scholar
Brown, G. (1953) The dioctahedral analogue of vermiculite. Clay Miner. Bull., 2, 64–69.Google Scholar
Bryant, J.P. & Dixon, J.B. (1963) Clay mineralogy and weathering of a red-yellow podzolic soil from quartz mica schist in the Alabama piedmont. Clays Clay Miner., 12, 509–521.Google Scholar
Carlisle, V.W. & Zelazny, L.W. (1973) Mineralogy of selected Florida Paleudults. Proc. Soil Crop Sci. Soc. Fla., 33, 136–139.Google Scholar
Douglas, L.S. (1989) Vermiculites. Pp. 635–674 in: Minerals in Soil Environments(J.B. Dixon & S.B. Weed, editors). Soil Sci. Soc. Am., Madison, Wisconsin.Google Scholar
Dixon, J.B. (1989) Kaolinite and serpentine group materials. Pp. 467-525 in: Minerals in Soil Environments (J.B. Dixon & S.B. Weed, editors). Soil Sci. Soc. Am., Madison, Wisconsin.Google Scholar
Farmer, V.C., Smith Wilson, M.J., Loveland, P.J. & Payton, R.W. (1988) Readily-extractable hydroxyaluminium interlayers in clay and silt-sized vermiculite. Clay Miner., 23, 271–277.Google Scholar
Frink, C.R. (1965) Characterization of aluminum interlayers in soil clays. Soil Sci. Soc. Am. Proc., 29, 379–382.CrossRefGoogle Scholar
Harris, W.G. & Carlisle, V.W. (1987) Clay mineralogical relationships in Florida Haplaquods. Soil Sci. Soc. Am. J., 51, 481–484.Google Scholar
Harris, W.G., Iyengar, S.S., Zelazny, L.W., Parker, J.C., Lietzke, D.A. & Edmonds, W.J. (1980) Mineralogy of a chronosequence formed in New River alluvium. Soil Sci. Soc. Am. J., 44, 862–868.Google Scholar
Hashimoto, I. & Jackson, M.L. (1960) Rapid dissolution of allophane and kaolinite-halloysite after dehydration. Clays Clay Miner., 7, 102–113.Google Scholar
Karathanasis, A.D. (1988) Compositional and solubility relationships between aluminum-hydroxyinterlayered soil-smectites and vermiculites. Soil Sci. Soc. Am. J., 52, 1500–1508.CrossRefGoogle Scholar
Kirkland, D.L. & Hajek, B.F. (1972) Formula derivation of Al-interlayered vermiculite in selected soil clays. Soil Sci., 114, 317–322.Google Scholar
MacEwan, D.M.C. (1950) Some notes on the recording and interpretation of X-ray diagrams of soil clays. J. Soil Sci., 1, 90–103.CrossRefGoogle Scholar
Mellor, A. & Wilson, M. J. (1987) Processes and products of mineral weathering in soils of the SWAP catchments in Scotland and Norway. Proc. SWAP Mid Term Review Conf. Roy. Soc. Lond., 98–105.Google Scholar
Norrish, K. & Hutton, J.T. (1969) An accurate X-ray spectrographic method for the analysis of a wide range of geological samples. Geochim. Cosmochim. Acta, 33, 431–453.Google Scholar
Olson, C.G. (1988) Clay-mineral contribution to the weathering mechanisms in two contrasting watersheds. J. Soil Sci., 39, 457–467.Google Scholar
Rich, C.I. (1968) Hydroxyinterlayers in expansible layer silicates. Clays Clay Miner., 16, 15–30.CrossRefGoogle Scholar
Rich, C.I. & Obenshain, S.S. (1955) Chemical and clay mineral properties of a red-yellow podzolic soil derived from muscovite schist. Soil Sci. Soc. Am. Proc., 19, 334–339.Google Scholar
Vicente, M.A., Razzaghe, M. & Robert, M. (1977) Formation of aluminium hydroxy vermiculite (intergrade) and smectite from mica under acidic conditions. Clay Miner., 12, 101–112.Google Scholar
Wilson, M.J. (1986) Mineral weathering processes in podzolic soils on granitic materials and their implications for surface water acidification. J. Geol. Soc. Lond., 143, 691–697.Google Scholar
Wilson, M.J., Bain, D.C. & Duthie, D.M.L. (1984) The soil clays of Great Britain: II. Scotland. Clay Miner., 19, 709–735.Google Scholar