PS 17-136
Lawn management effects on soil carbon quality

Monday, August 11, 2014
Exhibit Hall, Sacramento Convention Center
Paul J. Lilly, Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT
Jennifer C. Jenkins, Rubenstein School of Environment and Natural Resources, University of Vermont
Mark J. Carroll, Plant Science and Landscape Architecture, University of Maryland
Peter M. Groffman, Cary Institute of Ecosystem Studies, Millbrook, NY
Background/Question/Methods

Large intra-annual changes in soil C pools have been observed under turfgrass lawns, and lawns have been observed to substantially increase soil C pools under certain conditions.  In order to better understand these dynamics and determine any influence that lawn management might have on them, we conducted long-term (90+ days) incubations of soil collected from under tall fescue (Lolium arundinaceum (Schreb.) Darbysh.) managed to mimic a range of observed homeowner behaviors at several points throughout the growing season.  We used a three-pool model to generate estimates of fast-turnover, slow-turnover, and recalcitrant soil C pools.

Results/Conclusions

Differences in total soil C pools between sampling dates were larger than differences between management treatments, suggesting that a general pattern of rapid soil C accumulation in the spring, followed by gradual depletion over the course of the growing season dominates intra-annual dynamics.  However, each of our management variables (mowing height, irrigation, and fertilization) had significant (α=0.05) effects on the size of different soil C pools at different points in time, indicating that management can influence how C is processed in this system.  The ratio of fast-turnover to slow-turnover to recalcitrant soil C in this system appears to be weighted more heavily toward fast-turnover C than in other systems where this has been measured.