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.

Files

Institutions

University of California Santa Cruz

Categories

Rhizosphere, Soil Aggregate, Isotopic Tracer Data, Dissolved Organic Carbon, Agricultural Soil

Funders

  • National Science Foundation Division of Environmental Biology
    Grant ID: Grant No.DEB-1354098

Licence