Clay-salt soil formations in situ and ex situ View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2015-04

AUTHORS

G. V. Kharitonova, E. V. Shein, M. A. Pugachevskii, V. S. Komarova, Z. N. Tyugai, A. S. Manucharov, T. D. Ri

ABSTRACT

The methods of scanning and transmission electron microscopy, energy-dispersive analysis, and electron energy loss spectroscopy are used for the study of the interaction of soluble sodium and magnesium sulfates, as well as sodium chloride (in the presence of Na and Mg sulfates), with clay minerals: kaolinite and smectite. It is shown that the interaction of clay minerals with salt solutions initiates the reorganization of crystallites of the minerals and results in the formation of clay-salt microaggregates. The manifestation of the formation of clay-salt microaggregates and their composition, size, shape, and particle-packing state depend on the nature of the minerals and the properties of the salt participating in the interaction. In addition, the interaction of sodium chloride in the presence of sulfates results in the formation of peculiarly shaped pen tagonal clay–salt ultramicroaggregates. Their microdiffraction patterns are characterized by the presence of reflections corresponding to fivefold rotational symmetry; this may be evidence of their quasicrystalline structure. More... »

PAGES

50-57

Identifiers

URI

http://scigraph.springernature.com/pub.10.3103/s0147687415020027

DOI

http://dx.doi.org/10.3103/s0147687415020027

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1052422840


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