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Cohesion pressure in zeolite-water system

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Bulletin of the Academy of Sciences of the USSR, Division of chemical science Aims and scope

Conclusions

A change in the volume of the zeolite-water system, the same as of an electrolytewater system, is caused mainly by a change in the kinetic component of the internal (cohesion) pressure when the amount of water is varied.

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Authors and Affiliations

  1. Institute of Chemical Physics, Academy of Sciences of the USSR, Moscow

    G. I. Berezin & A. A. Kozlov

Authors
  1. G. I. Berezin
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  2. A. A. Kozlov
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Translated from Izvestiya Akademii Nauk SSSR, Seriya Khimicheskaya, No. 3, pp. 708–710, March, 1984.

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Berezin, G.I., Kozlov, A.A. Cohesion pressure in zeolite-water system. Russ Chem Bull 33, 658–661 (1984). https://doi.org/10.1007/BF00995721

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  • DOI: https://doi.org/10.1007/BF00995721

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