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dc.contributor.authorDaly, Edoardo
dc.contributor.authorPalmroth, Sari
dc.contributor.authorStoy, Paul C.
dc.contributor.authorSiqueira, Mario B. S.
dc.contributor.authorOishi, A. Christopher
dc.contributor.authorJuang, Jehn-Yih
dc.contributor.authorOren, Ram
dc.contributor.authorPorporato, Amilcare
dc.contributor.authorKatul, Gabriel G.
dc.date.accessioned2019-02-25T15:59:57Z
dc.date.available2019-02-25T15:59:57Z
dc.date.issued2009-05
dc.identifier.citationDaly, Edoardo, Sari Palmroth, Paul Stoy, Mario Siqueira, A. Christopher Oishi, Jehn-Yih Juang, Ram Oren, Amilcare Porporato, and Gabriel G. Katul. “The Effects of Elevated Atmospheric CO2 and Nitrogen Amendments on Subsurface CO2 Production and Concentration Dynamics in a Maturing Pine Forest.” Biogeochemistry 94, no. 3 (May 7, 2009): 271–287. doi:10.1007/s10533-009-9327-7.en_US
dc.identifier.issn1573-515X
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/15284
dc.description.abstractProfiles of subsurface soil CO2 concentration, soil temperature, and soil moisture, and throughfall were measured continuously during the years 2005 and 2006 in 16 locations at the free air CO2 enrichment facility situated within a temperate loblolly pine (Pinus taeda L.) stand. Sampling at these locations followed a 4 by 4 replicated experimental design comprised of two atmospheric CO2 concentration levels (ambient [CO2]a, ambient + 200 ppmv, [CO2]e) and two soil nitrogen (N) deposition levels (ambient, ambient + fertilization at 11.2 gN m−2 year−1). The combination of these measurements permitted indirect estimation of below ground CO2 production and flux profiles in the mineral soil. Adjacent to the soil CO2 profiles, direct (chamber-based) measurements of CO2 fluxes from the soil–litter complex were simultaneously conducted using the automated carbon efflux system. Based on the measured soil CO2 profiles, neither [CO2]e nor N fertilization had a statistically significant effect on seasonal soil CO2, CO2 production, and effluxes from the mineral soil over the study period. Soil moisture and temperature had different effects on CO2 concentration depending on the depth. Variations in CO2 were mostly explained by soil temperature at deeper soil layers, while water content was an important driver at the surface (within the first 10 cm), where CO2 pulses were induced by rainfall events. The soil effluxes were equal to the CO2 production for most of the time, suggesting that the site reached near steady-state conditions. The fluxes estimated from the CO2 profiles were highly correlated to the direct measurements when the soil was neither very dry nor very wet. This suggests that a better parameterization of the soil CO2 diffusivity is required for these soil moisture extremes.en_US
dc.description.sponsorshipOffice of Science (BER), U.S. Department of Energy, Grant no. DE-FG02-95ER62083en_US
dc.language.isoenen_US
dc.rightsThis Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.titleThe Effects of Elevated Atmospheric CO2 and Nitrogen Amendments on Subsurface CO2 Production and Concentration Dynamics in a Maturing Pine Foresten_US
dc.typeArticleen_US
mus.citation.extentfirstpage271en_US
mus.citation.extentlastpage287en_US
mus.citation.issue3en_US
mus.citation.journaltitleBiogeochemistryen_US
mus.citation.volume94en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1007/s10533-009-9327-7en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.data.thumbpage9en_US


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