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The nature of clinoptilolite from georgian beds

  • T. N. Ivanova
  • A. I. Sarakhov
  • M. M. Dubinin
Physical Chemistry
  • 19 Downloads

Conclusions

  1. 1.

    Study has been made of clinoptilolites from the Dzegvi and Khekardzula beds in Georgia, using x-ray and electron microscope microphotometric methods coupled with porisometric measurements.

     
  2. 2.

    The Khekardzula mineral consists of fine-grained crystalline clinoptilolite (≪ 1 μm) interspersed with coarse (∿5 μm) crystals of gypsum and heulandite. There is also the possibility that these samples contain a certain amount of an amorphous phase of unknown composition.

     

Keywords

Electron Microscope Gypsum Amorphous Phase Clinoptilolite Unknown Composition 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Literature cited

  1. 1.
    R. Wise, Amer. Min.,54, 887 (1969).Google Scholar
  2. 2.
    Collection: Natural Sorbents with Zeolite Structure [in Russian], Fan, Tashkent (1974).Google Scholar
  3. 3.
    M. M. Dubinin, N. S. Lozhkova, and B. A. Onusaitis, Izv. Akad. Nauk SSSR, Ser. Khim., 731 (1976).Google Scholar

Copyright information

© Plenum Publishing Corporation 1978

Authors and Affiliations

  • T. N. Ivanova
    • 1
  • A. I. Sarakhov
    • 1
  • M. M. Dubinin
    • 1
  1. 1.Institute of Physical ChemistryAcademy of Sciences of the USSRMoscow

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