Mineralogy and chemistry of finely dispersed bottom sediments in the Amur River View Full Text


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Article Info

DATE

2011-07-16

AUTHORS

N. P. Chizhikova, S. E. Sirotskii, G. V. Kharitonova, A. S. Manucharov, N. S. Konovalova, E. V. Utkina

ABSTRACT

The mineralogy and chemistry of the fine fractions separated from the bottom sediments (aquasols) in the Amur River were studied in the subfractions of the fractional peptization differing in the binding strength between the water-peptized and aggregated components. Detritus of quartz, field spars, and strongly degraded layered silicates mainly passes into the water-peptized state. Interstratified layered silicates with different combinations of chlorite and mica layers prevail in the aggregate subfraction. The distribution of the microelements in the bottom sediments, the water-peptized and aggregated clays, and the residues after their separation was determined. The content of iron, manganese, zinc, and copper in the clay subfractions was higher than in the bottom sediments and in the residue after the separation of the clay subfractions by 2–4 times, which confirmed the functional significance of the clay minerals. The presence of diatomic algae in the components of the bottom sediments was revealed by scanning electron microscopy. The contribution of the diatoms to the accumulation of iron, manganese, zinc, and copper was shown. More... »

PAGES

781-793

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1064229311070039

DOI

http://dx.doi.org/10.1134/s1064229311070039

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1003155753


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