Crystallochemical transformation of phyllosilicates under the impact of cyanobacteria and actinomycetes View Full Text


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Article Info

DATE

2009-01

AUTHORS

N. P. Chizhikova, E. O. Omarova, E. S. Lobakova, G. M. Zenova, A. S. Manucharov

ABSTRACT

The transformation of the crystallochemical structure of phyllosilicates (vermiculite and biotite) under the impact of growing cyanobacterial and actinomycetal associations, as well as monocultures of cyanobacteria and actinomycetes, has been studied. The character of the mineral transformation depends on their crystallochemical structure and the type of biota. The most significant changes take place in the contact zone between minerals and microbial associations; the effect of microbial monocultures is smaller. The transformation of biotite proceeds via the stage of ordered mica-vermiculite (smectite) neoformation (rectorite); the destruction of vermiculite has been identified. More... »

PAGES

69-74

References to SciGraph publications

  • 1988. Microbial Weathering Processes in Natural Environments in PHYSICAL AND CHEMICAL WEATHERING IN GEOCHEMICAL CYCLES
  • 1994-05. Enhanced dissolution of silicate minerals by bacteria at near-neutral pH in MICROBIAL ECOLOGY
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    http://scigraph.springernature.com/pub.10.1134/s1064229309010098

    DOI

    http://dx.doi.org/10.1134/s1064229309010098

    DIMENSIONS

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