SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 36:772-777 (1972)
© 1972 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 Google Scholar
Google Scholar
Right arrow Articles by Schnitzer, M.
Right arrow Articles by Riffaldi, R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Schnitzer, M.
Right arrow Articles by Riffaldi, R.
Agricola
Right arrow Articles by Schnitzer, M.
Right arrow Articles by Riffaldi, R.

The Determination of Quinone Groups in Humic Substances1

M. Schnitzer and R. Riffaldi2

ABSTRACT

The reduction of quinone groups in humic substances by acid SnCl2 solution was found to be unsatisfactory. The experimental conditions are drastic, the systems are heterogeneous, favoring adsorption or complexing of the reducing agent by the humic materials, and so leading to excessively high quinone values.

Reduction of humic substances by SnCl2 and Fe2+-triethanolamine in alkaline solution at room temperature and atmospheric pressure appeared to be more suitable for the determination of quinone groups in these materials. There was good agreement between quinone groups determined by the two methods on seven humic and one fulvic acid. The quinone group content of the humic acids analyzed ranged from 1.4 to 2.2 meq/g, that of the fulvic acid was < 1.0 meq/g.

No correlation was found between quinone groups and the free radical content of the humic materials. The results suggest that quinone groups in humic substances form part of complex chemical structures and not of simple compounds.

The determination of quinone groups in humic substances is difficult because of the presence of substantial amounts of CO2H, OH, and ketonic C=0 groups, some or all of which may interfere. Thus, it is advisable to check each analysis by at least two different methods.


NOTES

1 Contribution no. 406. Soil Research Institute, Canada Dep. of Agr., Ottawa, Ontario.

2 Senior Research Scientist and visiting Scientist from the Agr. Chemistry Institute, Univ. of Pisa, Pisa, Italy, respectively.

Received for publication January 26, 1972. Accepted for publication May 9, 1972.







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 © 1972 by the Soil Science Society of America.