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


     


Published online 29 October 2007
Published in Soil Sci Soc Am J 71:1934-1944 (2007)
DOI: 10.2136/sssaj2006.0283
© 2007 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
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 Campbell, J. L.
Right arrow Articles by Christenson, L. M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Campbell, J. L.
Right arrow Articles by Christenson, L. M.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Campbell, J. L.
Right arrow Articles by Christenson, L. M.
Related Collections
Right arrow Biogeochemical Processes
Right arrow Sulfur
Right arrow Nitrogen

FOREST, RANGE & WILDLAND SOILS

Mobility of Nitrogen-15-Labeled Nitrate and Sulfur-34-Labeled Sulfate during Snowmelt

John L. Campbella,*, Myron J. Mitchellb, Bernhard Mayerc, Peter M. Groffmand and Lynn M. Christensond

a U.S. Forest Service, PO Box 640, Durham, NH 03824
b State Univ. of New York, College of Environmental Science and Forestry, 1 Forestry Dr. Syracuse, NY 13210
c Univ. of Calgary, 2500 University Dr. NW, Calgary, AB, Canada T2N 1N4
d Institute of Ecosystem Studies, Box AB, Millbrook, NY 12545-0129

* Corresponding author (jlcampbell{at}fs.fed.us).

The objective of this study was to investigate the winter dynamics of SO42– and NO3 in a forested soil to better understand controls on these acidifying anions during snowmelt. In February 2004, a stable isotopic tracer solution with 93 atom% 34S as H234SO4 and 99 atom% 15N as NH415NO3 was applied to the snowpack at the Hubbard Brook Experimental Forest in New Hampshire. The chemical and isotopic compositions of throughfall, snow, snowmelt, and forest floor leachates were monitored for 10 mo following the addition of the tracers. The 34SO42– and 15NO3 tracer amounts in forest floor leachates were highest in the first fractions of meltwater and declined exponentially until returning to ambient levels in mid-May. Isotopic mass balances indicated that SO42– and NO3 were conservative in the snowpack, with tracer recoveries near 100%. In contrast, only 54 to 62% of the 34SO42– and 49 to 58% of the 15NO3 were recovered in forest floor leachates, suggesting that much of the SO42– and NO3 that infiltrated the forest floor during snowmelt was retained or transformed. Microbial biomass {delta}15N values in the forest floor remained low during snowmelt and the natural abundance values of {delta}18O–NO3 in forest floor leachates were indicative of an atmospheric rather than a microbial source. These results suggest that, in this study, microbial immobilization and subsequent mineralization and nitrification of snowpack NO3 was insignificant in the forest floor during snowmelt.

Abbreviations: DNRA, dissimilatory nitrate reduction to ammonia • HBEF, Hubbard Brook Experimental Forest • PVC, polyvinyl chloride







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 © 2007 by the Soil Science Society of America.