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


     


Published online 1 January 2007
Published in Soil Sci Soc Am J 71:108-117 (2007)
DOI: 10.2136/sssaj2005.0170
© 2007 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 Similar articles in ISI Web of Science
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 Matocha, C. J.
Right arrow Articles by Coyne, M. S.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Matocha, C. J.
Right arrow Articles by Coyne, M. S.
Agricola
Right arrow Articles by Matocha, C. J.
Right arrow Articles by Coyne, M. S.
Related Collections
Right arrow Redox Processes
Right arrow Biogeochemical Processes
Right arrow Soil Chemistry

SOIL CHEMISTRY

Short-term Response of Soil Iron to Nitrate Addition

C. J. Matocha*

Department of Plant and Soil Science, Univ. of Kentucky, N-122 Agricultural Science Center-North, Lexington, KY 40546-0091

M. S. Coyne

Department of Plant and Soil Science, Univ. of Kentucky, N-122 Agricultural Science Center-North, Lexington, KY 40546-009

* Corresponding author (cjmato{at}uky.edu).

The inhibition of soil Fe(III) reduction by fertilizer NO3 applications is complex and not completely understood. This inhibition is important to study because of the potential impact on soil physicochemical properties. We investigated the effect of adding NO3 to a moderately well-drained agricultural soil (Sadler silt loam) under Fe(III)-reducing (anoxic) conditions. Stirred-batch experiments were conducted where NO3 was added (0.05 and 1 mM) to anoxic slurries and changes in dissolved Fe(II) and Fe(III), oxalate-extractable Fe(II), and dissolved NO3 were monitored as a function of time. Addition of 1 mM NO3 inhibited Fe(II) production sharply with reaction time, from 10% after 1 h to 85% after 24 h. The duration of inhibition in Fe(II) production was closely related to the presence of available NO3, suggesting preferential use of NO3 by nitrate reductase enzyme. Active nitrate reductase was confirmed by the fivefold decline in NO3 reduction rates in the presence of tungstate (WO42–), a well-known inhibitor of nitrate reductase. In addition, NO3–dependent Fe(II) oxidation was observed to contribute to the inhibition in Fe(II) production. This finding was attributed to a combination of chemical reoxidation of Fe(II) by NO2– and NO3–dependent Fe(II) oxidation by autotrophic bacteria. These two processes became more important at a greater initial oxalate-Fe(II)/NO3 concentration ratio. The inhibitory effects in Fe(II) production were short-term in the sense that once NO3 was depleted, Fe(II) production resumed. These results underscore the complexity of the coupled N–Fe redox system in soils.




This article has been cited by other articles:


Home page
Soil Sci.Home page
S. Rakshit, C. J. Matocha, and M. S. Coyne
Nitrite Reduction by Siderite
Soil Sci. Soc. Am. J., June 18, 2008; 72(4): 1070 - 1077.
[Abstract] [Full Text] [PDF]




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
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2007 by the Soil Science Society of America.