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


     


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 ISI Web of Science (29)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Borken, W.
Right arrow Articles by Trumbore, S. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Borken, W.
Right arrow Articles by Trumbore, S. E.
Agricola
Right arrow Articles by Borken, W.
Right arrow Articles by Trumbore, S. E.
Related Collections
Right arrow Forest Soils
Published in Soil Sci. Soc. Am. J. 67:1888-1896 (2003).
© 2003 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

DIVISION S-7—FOREST & RANGE SOILS

Drying and Wetting Effects on Carbon Dioxide Release from Organic Horizons

W. Borken*,a,d, E. A. Davidsona, K. Savagea, J. Gaudinskib and S. E. Trumborec

a Woods Hole Research Center, P.O. Box 296, Woods Hole, MA 02543
b Dep. of Environmental Studies, Univ. of California, Santa Cruz, CA 95064
c Dep. of Earth System Science, Univ. of California, Irvine, CA 92697
d BITÖK, Bayreuther Institut für terrestrische Ökosystemforschung, Bayreuth, Germany

* Corresponding author (werner.borken{at}bitoek.uni-bayreuth.de).

Drying and wetting cycles of O horizon in forest soils have not received much attention, partly due to methodological limitations for nondestructive monitoring of the O horizon water content. The objective of this study was to determine the importance of moisture limitations in the O horizon of a temperate forest on summertime soil respiration. We measured soil respiration in three replicated plots in a mixed deciduous forest at Harvard Forest, Massachusetts, weekly from May to October 2001. Direct Current (DC) half-bridge sensors that had been calibrated using destructive samples of the Oi and Oe/Oa horizons were placed in the Oi and Oe/Oa horizons to record hourly changes of gravimetric water contents. Soil temperature explained 47% of the variation in soil respiration using the Arrhenius equation. The residuals of the temperature model were linearly correlated with gravimetric water content of the Oi horizon (r2 = 0.72, P < 0.0001) and Oe/Oa horizon (r2 = 0.56, P < 0.001), indicating that temporal variation in soil respiration can be partly explained by water content of the O horizon. Additionally, a laboratory study was performed to evaluate drying/wetting cycles of the O horizon at constant temperature. Even small simulated rainfall amounts of 0.5 mm significantly increase CO2 flux from dry O horizon within a few minutes. The duration of CO2 pulses increased with the amount of applied water, lasting from a few hours to days. A strong correlation between CO2 release and water content of the O horizons demonstrates a clear regulatory role of litter water content on decomposition within the O horizons.

Abbreviations: DC, direct current • IRGA, infrared gas analyzer • SOC, soil organic carbon • TDR, Time domain reflectometry







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 © 2003 by the Soil Science Society of America.