Managing Global Resources for a Secure Future

2017 Annual Meeting | Oct. 22-25 | Tampa, FL

108227 Soil Nitrogen Responses to an Ice Storm Manipulation Experiment in a Temperate Forested Ecosystem.

Poster Number 911

See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Forest, Range and Wildland Soils General Poster

Monday, October 23, 2017
Tampa Convention Center, East Exhibit Hall

Julie N. Weitzman and Peter M Groffman, Advanced Science Research Center, City University of New York, New York, NY
Abstract:
Temperate forest ecosystems are increasingly impacted by human-induced changes in climate, which have the ability to alter the prevalence, severity, and extent of extreme weather events. Ice storms, an example of such extreme events, tend to be rarer and often occur as localized events, making them difficult to predict. As such, their impacts on ecosystem structure and functioning are poorly understood. We utilized a field manipulation experiment that effectively simulated natural ice storms of varying intensities to mechanistically understand the short term nitrogen responses to such extreme weather events. Net N mineralization and nitrification were quantified for both the organic and mineral soil horizons via 30-day in situ incubations of intact soil cores, while gross N transformations were measured in short-term laboratory incubations using the 15N pool dilution technique. These microbial N transformation measurements were carried out in the fall of the pre-treatment year (2015), and the spring and fall of the post-treatment years (2016 and 2017). We found that the availability of inorganic N to the microbial community increased immediately following the simulated ice storms, and hypothesize that this is largely due to a decrease in plant uptake of inorganic N in response to canopy loss. Over longer time-scales we expect that N loss (mineralization, nitrification, denitrification) and conservation (immobilization) processes will be controlled more by the flow and availability of labile C from newly decaying fine and coarse woody debris that was dropped immediately following the ice storm.

See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Forest, Range and Wildland Soils General Poster