Hostname: page-component-cd9895bd7-dk4vv Total loading time: 0 Render date: 2024-12-24T02:56:10.219Z Has data issue: false hasContentIssue false

Characterization of Morphological Features of Soil Micas Using Scanning Electron Microscopy

Published online by Cambridge University Press:  01 July 2024

J. G. Tarzi
Affiliation:
Department of Land Resource Science, University of Guelph, Guelph, Ontario, Canada N1G 2W1
R. Protz
Affiliation:
Department of Land Resource Science, University of Guelph, Guelph, Ontario, Canada N1G 2W1
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.

Morphological changes occurring in naturally weathered micas in seven residual soils from Ontario were studied. Splitting, exfoliation of the (100) planes, surface coats, filling of spaces with soil material as well as cracking and crumbling of (001) surfaces were the main morphological changes found to be taking place during natural weathering of mica particles. The significance of the observed feature in relation to the general theory of mica weathering is discussed.

Резюме

Резюме

Изучались морфологические изменения,наблюдающиеся в естественно выветренных слюдах в семи образцах элювия,отобранных в Онтарио. Было обнаружено,что расщепление,расслаивание плоскостей/100/,поверхностные покровы,заполняющие промежутки почвенным материалом,также как растрескивание и смятие поверхностей/001/ были главными морфологическими изменениями,происшедшими в период естественного выветривания частиц слюды. Обсуждается значение выявленных особенностей для общей теории выветривания слюды.

Kurzreferat

Kurzreferat

Morphologische Veränderungen,welche in natürlich verwetterten Glimmern in sieben Eluvialböden in Ontario vorkommen,wurden untersucht.Spaltung, Abblätterung de. (100) Ebenen,Oberflächendecken,das Füllen von Plätzen mit Erdmaterial wie auch Brechen und Zerbröckeln vo. (001) Oberflächen waren die hauptsächlichen morphologischen Veränderungen,welche während der natürlichen Verwetterung der Glimmerteilchen Platz nehmen. Die Bedeutung der beobachteten Eigenschaften im Vergleich zu der allgemeinen Theorie der Glimmerteilchen wird diskutiert.

Résumé

Résumé

Les changements morphologiques survenant dans des micas naturellement altérés à l'air dans sept sols résiduels d'Ontario ont été étudiés. La fendaison et 1'exfoliation des plans(100), l'apparition de couches sur les surfaces, le remplissage d'espace de matière provenant du sol, ainsi que le craquement et l’émiettement des surfaces(001) étaient les principaux changements morphologiques survenant pendant l'altération naturelle des particules de mica à l'air. La signification de cette observation est discutée en relation avec la théorie générale de l'altération du mica.

Type
Research Article
Copyright
Copyright © 1978, The Clay Minerals Society

References

Arshad, M. A., St. Arnaud, R. J. and Huang, P. M. (1972) Dissolution of trioctahedral layer silicates by ammonium oxalate, sodium dithionite-citrate-bicarbonate, and potassium pyrophosphate: Can. J. Soil Sci. 25, 1925.CrossRefGoogle Scholar
Boyle, J. R., Voigt, G. K. and Sawhney, B. L. (1967) Biotite flakes: alteration by chemical and biological treatment: Science 155, 193195.CrossRefGoogle ScholarPubMed
Jackson, M. L., Lee, S. Y., Brown, J. L., Sachs, I. B. and Syers, J. K. (1973) Scanning electron microscopy of hydrous metal oxide crusts intercalated in naturally weathered micaceous vermiculite: Soil Sci. Soc. Am. Proc. 37, 127131.CrossRefGoogle Scholar
Jackson, M. L. and Sridhar, K. (1974) Scanning electron microscope and X-ray diffraction study of natural weathering of phlogopite through vermiculite to saponite: Soil Sci. Soc. Am. Proc. 38, 843847.CrossRefGoogle Scholar
Lee, S. Y., Jackson, M. L. and Sachs, I. B. (1974) Fission particle tracks in micas and micaceous vermiculites: Soil Sci. Soc. Am. Proc. 38, 423428.CrossRefGoogle Scholar
LeRoux, J. and Rich, C. I. (1969) Ion selectivity of micas as influenced by degree of potassium depletion: Soil Sci. Soc. Am. Proc. 33, 684690.CrossRefGoogle Scholar
MacKintosh, E. E., Lewis, D. G. and Greenland, D. J. (1971) Dodecylammonium-mica complexes—1. Factors affecting exchange reactions: Clays & Clay Minerals 19, 209218.CrossRefGoogle Scholar
McKeague, J. A. and Day, J. H. (1966) Dithionite- and oxalate-extractable Fe and Al as aids in differentiating various classes of soils: Can. J. Soil Sci. 46, 1322.CrossRefGoogle Scholar
Newman, A. C. D. and Brown, G. (1969) Delayed exchange of potassium from some edges of mica flakes: Nature 223, 175176.CrossRefGoogle Scholar
Protz, R. and St. Arnaud, R. J. (1964) The evaluation of four pretreatments used in particle-size distribution analyses: Can. J. Soil Sci. 44, 345351.CrossRefGoogle Scholar
Protz, R., Gillespie, J. E. and Brewer, R. (1974) Micromorphology and genesis of four soils derived from different rocks in Peterborough County, Ontario, Canada: Soil Microscopy, Proc. 4th Int. Working Meeting on Soil Micromorphology, Kingston, Ontario, pp. 481497.Google Scholar
Rausell-Colom, J. A., Sweatman, T. R., Wells, C. B. and Norrish, K. (1965) Studies in the artificial weathering of mica: Experimental Pedology, Proc. Univ. Nottingham 11th Easter Sch. Agric. Sci., pp. 4072.Google Scholar
Reichenbach, H. Graf von and Rich, C. I. (1969) Potassium release from moscovite as influenced by particle size: Clays & Clay Minerals 17, 2329.CrossRefGoogle Scholar
Rich, C. I. (1968) Mineralogy of soil potassium. In The Role of Potassium in Agriculture (Edited by Kilmer, V. J., Founts, S. E. and Brady, N. C.) , pp. 79108. Am. Soc. Agron., Crop Sci. Am., Soil Sci. Soc. Am.Google Scholar
Roth, C. B., Jackson, M. L., De Villiers, J. M. and Volk, V. V. (1966) Surface colloids on micaceous vermiculite: Trans. Comm. II & IV, Int. Soc. Soil Sci., Aberdeen, pp. 217221.Google Scholar
Roth, C. B., Jackson, M. L., Lotse, E. G. and Syers, J. K. (1968) Ferrous-ferric ratio and CEC changes on deferration of weathered micaceous vermiculite: Isr. J. Chem. 6, 261273.CrossRefGoogle Scholar
Scott, A. D. (1968) Effect of particle size on interlayer potassium from soils and micaceous minerals with solutions containing sodium tetraphenylboron: II. Biotite: Soil Sci. Soc. Am. Proc. 26, 4148.CrossRefGoogle Scholar
Scott, A. D. and Smith, S. J. (1967) Visible changes in macro mica particles that occur with potassium depletion: Clays & Clay Minerals, Proc. 15th Nat. Conf. pp. 6981.Google Scholar
Seddoh, F. K. and Robert, M. (1972) Intérêt de l'utilisation due microscope électronique à balayage pour l'étude des micas et de leur évolution (évolution expérimentale et dans le milieu naturel): Bull. Soc. Fr. Mineral. Cristallogr. 95, 7583.Google Scholar
Tarzi, J. G. (1976) Weathering of mica minerals in selected Ontario soils: Unpublished Ph.D. Thesis, Land Resource Science, University of Guelph, Guelph, Ontario.Google Scholar
Tarzi, J. G. and Protz, R. (1978) Increased selectivity of naturally weathered biotites for potassium: Soil Sci. Soc. Am. Proc. (submitted for publication).CrossRefGoogle Scholar
Wells, C. B. and Norrish, K. (1968) Accelerated rates of release of interlayer potassium from micas. Trans. 9th Int. Congr. Soil Sci. Adelaide, Australia, 2, 683694Google Scholar