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


     


Published in J Environ Qual 14:580-584 (1985)
© 1985 American Society of Agronomy, Crop Science Society of America, and 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
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Sims, G. K.
Right arrow Articles by Sommers, L. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Sims, G. K.
Right arrow Articles by Sommers, L. E.
Agricola
Right arrow Articles by Sims, G. K.
Right arrow Articles by Sommers, L. E.

Degradation of Pyridine Derivatives in Soil1

Gerald K. Sims and Lee E. Sommers2

ABSTRACT

The fate of pyridine and 25 substituted pyridines in soil (Aeric Ochraqualfs) was examined by measuring the quantity remaining and the inorganic N released as a result of degradation of the pyridine ring for a period of 64 d. Each compound was added to soil at 2 mmol kg–1. Compounds studied included pyridine substituted with one or two hydroxyl, carboxyl, chlorine, amine, or methyl groups. During the 64-d incubation period, extractability of pyridine derivatives with 2 M KCl + 0.01 M HC1 decreased from an average of 88 ± 8.8% to essentially 0 for all compounds except aminopyridines. From 36 to 94% of added aminopyridines was recovered after 64 d of incubation. Degradation of the majority of pyridine derivatives was confirmed by accumulation of N in amounts equivalent to 61 to 80% of the decrease in extractable pyridines at 64 d of incubation. Degradation of unsubstituted pyridine occurred within 8 d, whereas most hydroxypyridines were degraded within 32 to 64 d. Pyridinecarboxylic acids appear to be the most labile group of pyridine derivatives and were dissipated from soil in 4 to 16 d. Most chloropyridines persisted in soil and became weakly associated with some insoluble soil component. However, 4-chloropyridine degraded in 16 d. Aminopyridines resisted degradation in soil while methylpyridines were degraded in 8 to 32 d. Degradability of the compounds generally followed the order pyridinecarboxylic acids > pyridine = mono-hydroxypyridines > methylpyridines > aminopyridines and chloropyridines. This trend was consistent with previous results on biodegradability of the compounds in soil suspension cultures.

Key Words: lutidines • biodegradation • aminopyridine • hydroxypyridine • chloropyridine • pyridinecarboxylic acids


NOTES

1 Contribution from the Purdue Agric. Exp. Stn., West Lafayette, IN 47907, Journal Paper no. 10,386.

2 Graduate research assistant and professor, Dep. of Agronomy, Purdue Univ., West Lafayette, IN. The senior author is now assistant professor, Dep. of Agronomy, Ohio State Univ., Columbus, OH 43210.

Received for publication May 7, 1985.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Soil Science Society of America Journal Journal of Plant Registrations The Plant Genome
Copyright © 1985 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.