Diffusion and Conduction in Zeolites : Data compilation / edited by D.J. Fisher.

Contributor(s):

Fisher, D. J [editor.]

Material type: Text

TextSeries: Diffusion and defect data. Pt. A, Defect and diffusion forum ; ; v. 351.Publisher: [Place of publication not identified] : Trans Tech Publications, Ltd., [2014]Description: 1 online resourceContent type:

text

Media type:

computer

Carrier type:

online resource

ISBN:

9783038264613
303826461X

Subject(s): Genre/Form:

Additional physical formats: Print version:: Diffusion and Conduction in Zeolites.DDC classification:

620.116 23

LOC classification:

TA418.9.P6

Online resources:

Click here to access online

Contents:

Diffusion and Conduction in Zeolites; Table of Contents; Abstracts

Summary: The microporous aluminosilicate minerals known as Zeolites are invaluable as adsorbents, molecular sieves and catalysts because they possess a porous structure that can let pass or accommodate cations such as, Ca2+, K+, Mg2+, Na+, etc. These are nevertheless loosely held and can be easily exchanged for those in an adjacent solution. Movement of other materials through Zeolites is naturally an important factor. The present compilation consists of diffusion data. These represent, as far as possible, pure diffusion, shorn of other transfer mechanisms such as permeation. Most of the results involv.

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Includes abstracts of papers published in scientific literature.

Includes bibliographical references.

Online resource; title from HTML table of contents page (Scientific.Net, viewed July 30, 2014).

Diffusion and Conduction in Zeolites; Table of Contents; Abstracts

The microporous aluminosilicate minerals known as Zeolites are invaluable as adsorbents, molecular sieves and catalysts because they possess a porous structure that can let pass or accommodate cations such as, Ca2+, K+, Mg2+, Na+, etc. These are nevertheless loosely held and can be easily exchanged for those in an adjacent solution. Movement of other materials through Zeolites is naturally an important factor. The present compilation consists of diffusion data. These represent, as far as possible, pure diffusion, shorn of other transfer mechanisms such as permeation. Most of the results involv.

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