Tight coupling between photosynthesis and soil carbon turnover indicative of rhizosphere priming in the field

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dc.contributor.authorMcCloskey, Chris
dc.contributor.authorKirk, Guy J. D.
dc.contributor.authorOtten, Wilfred
dc.contributor.authorPaterson, Eric
dc.date.accessioned2022-05-24T10:21:25Z
dc.date.available2022-05-24T10:21:25Z
dc.date.issued2022-05-27
dc.descriptionAbstract only
dc.description.abstractWhile rhizosphere priming effects are well-documented under laboratory and controlled-environment conditions, their significance in undisturbed systems under field conditions is less clear. This is in part because it is impracticable to measure rates of rhizodeposition in the field with high resolution over a substantial period. We propose that photosynthesis, closely linked to rhizodeposition, can be used as a proxy for plant root activity.en_UK
dc.identifier.citationMcCloskey C, Kirk G, Otten W, Paterson E. (2022) Tight coupling between photosynthesis and soil carbon turnover indicative of rhizosphere priming in the field. In: EGU General Assembly, 2022, 23-27 May 2022, Vienna, Austria. Paper number EGU22-12193en_UK
dc.identifier.urihttps://doi.org/10.5194/egusphere-egu22-12193
dc.identifier.urihttp://dspace.lib.cranfield.ac.uk/handle/1826/17953
dc.language.isoenen_UK
dc.publisherEGU: European Geophysical Unionen_UK
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.titleTight coupling between photosynthesis and soil carbon turnover indicative of rhizosphere priming in the fielden_UK
dc.typeConference paperen_UK

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