SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 56:1784-1788 (1992)
© 1992 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Elprince, A. M.
Right arrow Articles by Mohamed, W. H.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Elprince, A. M.
Right arrow Articles by Mohamed, W. H.
Agricola
Right arrow Articles by Elprince, A. M.
Right arrow Articles by Mohamed, W. H.

Catalytic Decomposition Kinetics of Aqueous Hydrogen Peroxide and Solid Magnesium Peroxide By Birnessite

A. M. Elprince*

Kuwait Institute for Scientific Research, P.O. Box 24885, Safat 13109, Kuwait

W. H. Mohamed

Dep. of Soils and Agricultural Chemistry, Alexandria Univ., Alexandria, Egypt

* Corresponding author.

ABSTRACT

Peroxides are used as O2-generating agents. The decomposition of H2O2 (aq) or MgO2(s) in the presence of synthetic birnessite [{delta}-MnO2(s)] as a catalyst was observed by measuring the volume of O2(g) given off. The experimental data fit a first-order kinetic law and the mechanism proposed by Habes and Weiss can explain the experimental results obtained for the decomposition of H2O2(aq). The applicability of the proposed mechanism involving H2O2(aq) was based on the following: (i) the activation energy was relatively high (82 ± 3 kJ mol–1); (ii) the rate constant (k) was pH dependent, indicating that H+ and OH- ions were formed in the process; (iii) a linear relationship (and not logarithmic) between k and the ionic strength indicated a reaction between an ion and a neutral molecule; and (iv) using birnessite with different fractional coverages of Co indicated that the reaction was heterogeneously catalyzed by Mnz+1/Mnz active centers. Regarding MgO2(s) decomposition, the experimental data obtained at pH 7.6 followed a rate law derived from a shrinking-core model for fixed-size particles. The rate of the reaction was controlled by diffusion through the Mg(OH)2(s) product layer rather than by chemical reaction at the core surface. Compared with ionic peroxides, MgO2(s) could be a potential O2-generating agent for generating O2(g) during a relatively long period of time.

Received for publication August 5, 1991.


This article has been cited by other articles:


Home page
Soil Sci.Home page
A. M. Elprince, W. H. Mohamed, and E. M. El-Wakil
Kinetics of Nonenzymatic Decomposition of Hydrogen Peroxide by Torrifluvents
Soil Sci. Soc. Am. J., January 11, 2008; 72(1): 83 - 89.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1992 by the Soil Science Society of America.