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Reduction of forest floor respiration by fertilization on both carbon dioxide‐enriched and reference 17‐year‐old loblolly pine stands

JOHN R. BUTNOR; KURT H. JOHNSEN; RAM OREN; GABRIEL G. KATUL
Global Change Biology · Vol. 9, Issue 6 · pp. 849-861 · 2003

Abstract

Elevated atmospheric carbon dioxide (CO 2 e ) increases soil respiration rates in forest, grassland, agricultural and wetland systems as a result of increased growth, root biomass and enhanced biological activity of soil microorganisms. Less is known about how forest floor fluxes respond to the combined effects of elevated CO 2 and nutrient amendments; until now no experiments have been in place with large forest trees to allow even preliminary investigations. We investigated changes in forest floor respiration (S ff ) in a Pinus taeda L. plantation fumigated with CO 2 by using free‐air CO 2 enrichment (FACE) technology and given nutrient amendments. The prototype FACE apparatus (FACEp; 707 m 2 ) was constructed in 1993, 10 years after planting, on a moderate fertility site in Duke Forest, North Carolina, USA, enriching the stand to 55 Pa (CO 2 e ). A nearby ambient CO 2 (CO 2 a ) plot (117 m 2 ) was designated at the inception of the study as a reference (Ref). Both FACEp and Ref plot were divided in half and urea fertilizer was applied to one half at an annual rate of 11.2 g N m −2 in the spring of 1998, 1999 and 2000. Forest floor respiration was monitored continuously for 220 days – March through November 2000 – by using two Automated Carbon Efflux Systems. Thirty locations (491 cm 2 each) were sampled in both FACEp and Ref, about half in each fertility treatment. Forest floor respiration was strongly correlated with soil temperature at 5 cm. Rates of S ff were greater in CO 2 e relative to CO 2 a (an enhancement of ∼178 g C m −2 ) during the measurement period. Application of fertilizer resulted in a statistically significant depression of respiration rates in both the CO 2 a and CO 2 e plots (a reduction of ∼186 g C m −2 ). The results suggest that closed canopy forests on moderate fertility sites cycle back to the atmosphere more assimilated carbon (C) than similar forests on sites of high fertility. We recognize the limitations of this non‐replicated study, but its clear results offer strong testable hypotheses for future research in this important area.

Bibliographic Information

JournalGlobal Change Biology
PublisherWiley
Publication Date2003-06-01
Publication Year2003
Volume9
Issue6
Pages849-861
Document TypeJournal Article
Print ISSN1354-1013
eISSN1365-2486
DOI10.1046/j.1365-2486.2003.00630.x
SubjectConservation Science

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NARA Access Coverage1997-01-01~Current
Journal Homepagehttps://onlinelibrary.wiley.com/loi/13652486
Publisher PageOpen Publisher Page
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