Hostname: page-component-848d4c4894-x5gtn Total loading time: 0 Render date: 2024-06-01T00:31:10.981Z Has data issue: false hasContentIssue false

Clay-Organic Complexes as a Cementing Agent in the Arahama Sand Dune, Japan

Published online by Cambridge University Press:  02 April 2024

Kazue Tazaki
Affiliation:
Department of Geology, Shimane University, Nishikawatsu, Matsue, Shimane 690, Japan
S. Kimura
Affiliation:
Toyosaka High School, Toyosaka, Niigata 950-33, Japan
T. Yoshimura
Affiliation:
Department of Geology and Mineralogy, Niigata University, Ikarashi, Niigata 950-21, Japan
J. Akai
Affiliation:
Department of Geology and Mineralogy, Niigata University, Ikarashi, Niigata 950-21, Japan
W. S. Fyfe
Affiliation:
Department of Geology, University of Western Ontario, London, Ontario, N6A 5B7, Canada

Abstract

Cementing materials in the Arahama sand dune, Japan, were studied mineralogically and biogeochemically to gain a better understanding of the cause of hardening. The cementing material is a clay-organic complex composed of noncrystalline gels and a matrix of small, poorly crystalline particles showing 14–16-Å spacings. The gel materials appear to have transformed into the poorly crystalline particles, which have a high carbon content and Al/Si ratios of 2.2 to 2.0. These particles are slightly richer in Si and poorer in Fe than the gel materials themselves. The organic portion of the complex can be removed by H2O2 treatment, leaving a noncrystalline network-structure containing a dispersed granular component. Scanning auger-depth profiles of individual particles show a high surface concentration of C and O and an increase in the Al/Si ratio with depth. The energy-intensity distribution suggests a mixture of carbon compounds having a major core-line binding energy of a hydrocarbon. The gel-cementing materials in the sand dune may have been formed from biochemical weathering products of organic matter, which subsequently controlled the formation of clay-organic complexes.

Type
Research Article
Copyright
Copyright © 1989, The Clay Minerals Society

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.)

References

Berthelin, J. and Munier-Lamy, C., 1983 Microbial mobilization and preconcentration of uranium from various rock materials by fungi Ecol. Bull 35 395401.Google Scholar
Bond, R. D. and Harris, J. R., 1964 The influence of the microflora on the physical properties of soils. I. Effects associated with filamentous algae and fungi Aust. J. Soil Res 2 111122.CrossRefGoogle Scholar
Clark, D. T., Cromarty, B. J. and Dilks, A., 1978 A theoretical investigation of molecular core binding and relaxation energies in a series of oxygen-containing organic molecules of interest in the study of surface oxidation of polymers J. Polymer Science, Polymer Chem. Ed 16 31733184.CrossRefGoogle Scholar
Farmer, V. C., 1981 Possible roles of a mobile hydroxy-aluminum orthosilicate complex (proto-imogolite) and other hydroxyaluminum and hydroxy-iron species in podzolization Migrations Organo-Minerales dans les Sols Tempères Nancy, France Centre National de la Recherche Scientifique 275279.Google Scholar
Huang, P. M., Violante, A., Huang, P. M. and Schnitzer, M., 1986 Influence of organic acids on crystallization and surface properties of precipitation products of aluminum Interaction of Soil Minerals with Natural Organics and Microbes Madison, Wisconsin Soil Science Society of America 159221.CrossRefGoogle Scholar
Inoue, K. and Huang, P. M., 1986 Influence of selected organic ligands on the formation of allophane and imogolite Soil Sci. Soc. Amer. J 50 16231633.CrossRefGoogle Scholar
Nagarajah, S., Posner, A. M. and Quirk, J. P., 1970 Competitive adsorption of phosphate with polygalacturonate and other organic anions on kaolinite and oxide surfaces Nature (London) 228 8384.CrossRefGoogle ScholarPubMed
Niigata Ancient Dune Research Group, 1967 Ancient dunes along the coast of the Japan Sea Quaternary Res 6 1928.CrossRefGoogle Scholar
Research Group of Harden Soil, 1984 Characterization of the harden sand layer in Omiya, Japan Earth Science (Chikyu kagaku) 38 1730.Google Scholar
Ross, G. J. and Kodama, H., 1979 Evidence for imogolite in Canadian soils Clays & Clay Minerals 27 297300.CrossRefGoogle Scholar
Spyridakis, D. E., Chester, G. and Wilde, S. A., 1967 Kaolinization of biotite as a result of coniferous and deciduous seedling growth Soil Sci. Soc. Amer. Proc 31 203210.CrossRefGoogle Scholar
Tazaki, K., 1979 Scanning electron microscopic study of imogolite formation from plagioclase Clays & Clay Minerals 27 209212.CrossRefGoogle Scholar
Tazaki, K., Sudo, T., Shimoda, S., Yotsumoto, H. and Aida, S., 1980 Imogolite formed on weathered plagioclase Electron Micrographs of Clay Minerals Tokyo Kodansya 197199.Google Scholar
Tazaki, K., Lindenmayer, Z. G. and Fyfe, W. S., 1988 Formation of ultra-thin Cu-S films on minerals: A weathering product from silicate-facies iron formation, Salobo, Carajas, Brazil Chem. Geol 67 285294.CrossRefGoogle Scholar
Wada, K., Dixon, J. B. and Weed, S. B., 1977 Allophane and imogolite Minerals in Soil Environments Madison, Wisconsin Soil Science Society of America 603638.Google Scholar
Wada, K. and Theng, B. K. G., 1980 Mineralogical characteristics of Andisols Soils with Variable Charge Lower Hutt, New Zealand New Zealand Soc. Soil Sci- 8790.Google Scholar
Wada, K., Wilson, M., Kakuto, Y. and Wada, S., 1988 Synthesis and characterization of a hollow spherical form of monolayer aluminosilicate Clays & Clay Minerals 36 1118.CrossRefGoogle Scholar