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


     


Published online 5 April 2007
Published in Soil Sci Soc Am J 71:836-842 (2007)
DOI: 10.2136/sssaj2006.0339
© 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 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 Vourlitis, G. L.
Right arrow Articles by Mustard, R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Vourlitis, G. L.
Right arrow Articles by Mustard, R.
Agricola
Right arrow Articles by Vourlitis, G. L.
Right arrow Articles by Mustard, R.
Related Collections
Right arrow Dryland Soils
Right arrow Nitrogen
Right arrow Soil Organic Matter
Right arrow Global Change
Right arrow Nutrient Cycling

FOREST, RANGE & WILDLAND SOILS

Chronic Nitrogen Deposition Enhances Nitrogen Mineralization Potential of Semiarid Shrubland Soils

George L. Vourlitis*, Gypsi Zorba, Sarah C. Pasquini and Robert Mustard

Dep. of Biological Sciences, California State Univ., San Marcos, CA 92096

* Corresponding author (georgev{at}csusm.edu).

Semiarid chaparral and coastal sage shrublands of southern California have been exposed to high levels of atmospheric N for decades, which has the capacity to increase both N and C storage and cycling in these N-limited systems. Thus we hypothesize that soil C and N mineralization will be higher in areas that have been exposed to high atmospheric N deposition. This hypothesis was tested in a 50-wk laboratory incubation experiment where the inorganic N (NH4 + NO3) and CO2 production of chaparral and coastal sage soils were repeatedly measured. Soil was incubated in the dark at a constant temperature of 25°C and a soil moisture of 0.25 kg H2O kg–1 dry soil (65% water-filled pore space). Relative differences in N deposition exposure between the study sites were quantified by repeatedly rinsing and collecting the N accumulated on branch surfaces during 1 yr. Temporal trends in cumulative C and N mineralization were best described by single-pool first-order and zero-order models, respectively. Total N mineralization, but not C mineralization, increased linearly with relative N deposition, and NO3 accounted for 95% of the total inorganic N accumulated during the 50-wk incubation. The soil {delta}15N natural abundance increased with relative N deposition (r = 0.85, P < 0.05) and the soil C/N ratio declined with relative N deposition (r = –0.74, P < 0.05), suggesting that N deposition exposure enhanced N mineralization in part because of increases in the soil organic matter quality (i.e., lower C/N ratio). Furthermore, soil C storage declined as a function of relative N deposition exposure, indicating that high atmospheric N inputs are not likely to stimulate soil C storage in these semiarid ecosystems.

Abbreviations: {delta}15N, ratio of 15N/14N of a sample relative to a standard • MRR, Motte Rimrock Reserve • SDEF, San Dimas Experimental Forest • SLW, specific leaf weight • SMER, Santa Margarita Ecological Reserve • SOFS, Sky Oaks Field Station







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.