4.6 Article

Energetics of Alkali and Alkaline Earth Ion-Exchanged Zeolite A

Journal

JOURNAL OF PHYSICAL CHEMISTRY C
Volume 120, Issue 28, Pages 15251-15256

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/acs.jpcc.6b04840

Keywords

-

Funding

  1. U.S. Department of Energy, Office of Basic Energy Sciences [DE-FG02-05ER15667]
  2. Natural Science Foundation of Shanghai [16ZR1408100]
  3. China Scholarship Council [201308310077]
  4. Gene and Linda Voiland School of Chemical Engineering and Bioengineering at Washington State University

Ask authors/readers for more resources

Alkali and alkaline earth ion-exchanged zeolite A samples were synthesized in aqueous exchange media. They were thoroughly studied by powder X-ray diffraction (XRD), electron microprobe (EMPA), thermogravimetric analysis and differential scanning calorimetry (TG-DSC), and high temperature oxide melt solution calorimetry. The hydration energetics and enthalpies of formation of these zeolite A materials from constituent oxides were determined. Specifically, the hydration level of zeolite A has a linear dependence on the average ionic potential (Z/r) of the cation, from 0.894 (Rb-A) to 1.317 per TO2 (Mg-A). The formation enthalpies from oxides (25 degrees C) range from -93.71 +/- 1.77 (K-A) to -48.02 +/- 1.85 kJ/mol per TO2 (Li-A) for hydrated alkali ion-exchanged zeolite A, and from -47.99 +/- 1.20 (Ba-A) to -26.41 +/- 1.71 kJ/mol per TO2 (Mg-A) for hydrated alkaline earth ion-exchanged zeolite A. The formation enthalpy from oxides generally becomes less exothermic as Z/r increases, but a distinct difference in slope is observed between the alkali and the alkaline earth series.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.6
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available