Managing Global Resources for a Secure Future

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

207-3 Decadal Fate of a 15N Tracer in a Mixed Deciduous Forest.

See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Symposium--New Insights on Biogeochemical Processes in Terrestrial Ecosystems As Revealed By Isotopic and Biomarker Approaches I

Tuesday, October 24, 2017: 10:15 AM
Marriott Tampa Waterside, Florida Salon I-III

Christine Goodale, Ecology and Evolutionary Biology, Cornell University, Ithaca, NY and Carmen Enid Martinez, Soil and Crop Sciences, Cornell University, Ithaca, NY
Abstract:
The impacts of atmospheric nitrogen deposition on forest ecosystems depend on its fate. Past tracer studies show that litter and soils dominate the short-term fate of added 15N, yet few have examined longer-term dynamics or differences among forest types. This study is examining the decadal fate of a 15N-NO3- tracer in a stand evenly composed of trees with ectomycorrhizal and arbuscular mycorrhizal associations. The tracer was expected to slowly mineralize from its main initial fate in litter and surface soil, with some 15N moving to trees, some to deeper soil, and some net losses. Analyses for years 1 and 5-6 are complete, and year 10 sampling is scheduled for summer 2017. Recovery of added 15N in trees and litterfall totaled 11.3% at both year 1 and 5-6, as 15N redistributed from fine and especially coarse roots into litterfall, with small accumulations in woody tissues. Tree 15N acquisition occurred within the first year after the tracer addition, with no additional net transfer of 15N from detrital to plant pools by year 5-6. Ectomycorrhizal trees gained 50% more of the tracer than trees with arbuscular mycorrhizae at both timepoints. Tracer recovery rapidly decreased over time in surface litter material and accumulated in shallow and deep soil, perhaps through earthworm mixing. Overall, results showed redistribution of tracer 15N through trees and surface soils without any losses, as whole-ecosystem recovery remained constant between years 1 and 5-6 at 70% of the 15N addition. These results demonstrate persistent ecosystem retention of N deposition even as it redistributes, without additional plant uptake over this timescale. New sampling of the tracer’s fate at year 10 will allow investigation of whether 15N eventually turns over from detrital pools to become available to plants over decadal timescales, and how tree species differ in their ability to acquire this N.

See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Symposium--New Insights on Biogeochemical Processes in Terrestrial Ecosystems As Revealed By Isotopic and Biomarker Approaches I