13C differentiation of the dissolved organic carbon pool during carbon mineralization in soil from a native deciduous forest and a coniferous plantation

Gauthier, A., Amiotte-Suchet, P., Henault, C., Leveque, J., Nelson, P., and Ranger, J. (2007) 13C differentiation of the dissolved organic carbon pool during carbon mineralization in soil from a native deciduous forest and a coniferous plantation. In: Proceedings of International Symposium on Forest Soils and Ecosystem Health, pp. 31-32. From: International Symposium on Forest Soils and Ecosystem Health, 19-23 August 2007, Noosa, QLD, Australia.

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Abstract

Dissolved organic carbon (DOC) is a dynamic component of ecosystem functioning and environmental quality. This study demonstrates that different DOC dynamics (mineralization rates, δ13C) occur in forest soils either maintained as native or planted with Douglas fir.

Item ID: 8330
Item Type: Conference Item (Presentation)
Keywords: dissolved organic carbon; Douglas fir plantation; native forest; stable isotopes; soil organic matter; soil solution
ISBN: 978-1-921291-16-6
Date Deposited: 24 Feb 2010 03:59
FoR Codes: 05 ENVIRONMENTAL SCIENCES > 0503 Soil Sciences > 050303 Soil Biology @ 100%
SEO Codes: 96 ENVIRONMENT > 9614 Soils > 961403 Forest and Woodlands Soils @ 100%
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