The project described here seeks to answer questions regarding the role increased nitrogen (N) deposition is playing in enhanced carbon (C) sequestration in temperate mid-latitude forests, using detailed measurements from an AmeriFlux tower in southern Indiana (Morgan-Monroe State Forest, or MMSF). The measurements indicate an average atmosphere-surface N flux of approximately 6 mg-N m(-2) day(-1) during the 2000 growing season, with approximately 40% coming from dry deposition of ammonia (NH3), nitric acid (HNO3), and particle-bound N. Wet deposition and throughfall measurements indicate significant canopy uptake of N (particularly NH4+) at the site, leading to a net canopy exchange (NCE) of -6 kg-N ha(-1) for the growing season. These data are used in combination with data on the aboveground C:N ratio, litterfall flux, and soil net N mineralization rates to indicate the level of potential perturbation of C sequestration at this site.
CITATION STYLE
Pryor, S. C., Barthelmie, R. J., Carreiro, M., Davis, M. L., Hartley, A., Jensen, B., … Schoof, J. T. (2001). Nitrogen deposition to and cycling in a deciduous forest. TheScientificWorldJournal, 1 Suppl 2, 245–254. https://doi.org/10.1100/tsw.2001.372
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