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Ion exchange in the synthetic gismondine, zeolite MAP

Allen, S; Carr, S; Chapple, A; Dyer, A; Heywood, B

Authors

S Allen

S Carr

A Chapple

A Dyer

B Heywood



Abstract

Ion exchange has been studied in zeolite MAP, a synthetic gismondine used as a commercial detergent builder. The zeolite was fully characterized and shown to be a stable phase throughout the three year period of study. The ions pairs examined were; Na<->Li,K,Rb,Cs and Na<->½ Mg,Ca,Sr,Ba. All cation forms prepared were examined by powder X-ray diffraction (PXRD), magic-angle spinning (MAS) NMR and thermal analysis. When cation exchanges were shown to be reversible their isotherms were analysed to produce thermodynamic data. The values were then compared with literature values obtained for similar zeolite exchanges. Structural data (PXRD, MASNMR) showed that cation exchange often caused changes in unit cell symmetry as well as the creation of immiscible phases rich in the end-members when calcium and strontium were the in-going cations.

Citation

Allen, S., Carr, S., Chapple, A., Dyer, A., & Heywood, B. (2002). Ion exchange in the synthetic gismondine, zeolite MAP. Physical Chemistry Chemical Physics, 4(11), 2409-2415. https://doi.org/10.1039/b111490p

Journal Article Type Article
Publication Date May 2, 2002
Deposit Date Sep 3, 2007
Journal Physical Chemistry Chemical Physics
Print ISSN 1463-9076
Publisher Royal Society of Chemistry
Peer Reviewed Peer Reviewed
Volume 4
Issue 11
Pages 2409-2415
DOI https://doi.org/10.1039/b111490p
Publisher URL http://dx.doi.org/10.1039/b111490p


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