Linking the rhizosphere priming effect with soil aggregates, dissolved organic carbon, and leachable clay particles
Published: 27 July 2024| Version 1 | DOI: 10.17632/8mt5pzpmv6.1
Contributors:
Kelsey Forbush, Description
Soybeans were grown at three planting densities in a continuous 13C-isotope labeling greenhouse. We quantified the rhizosphere priming effect (RPE), water stable aggregate fractions, dissolved organic carbon (DOC), and clay particle concentrations in the leachate at five and eight weeks after planting.
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Institutions
University of California Santa Cruz
Categories
Rhizosphere, Soil Aggregate, Isotopic Tracer Data, Dissolved Organic Carbon, Agricultural Soil
Funding
National Science Foundation Division of Environmental Biology
Grant No.DEB-1354098