Hydrologic controls on the transport and cycling of carbon and nitrogen in a boreal catchment underlain by continuous permafrost. Issue 2 (13th May 2013)

• Record Type: Journal Article
• Authors: Koch, J. C.; Runkel, R. L.; Striegl, R.; McKnight, D. M.
• Is Part Of: Journal of geophysical research. Volume 118:Issue 2(2013:Jun.)
• Page Start: 698
• Page End: 712
• Publication Date: 2013-05-13
• Subjects: carbon -- nitrogen -- transient storage modeling -- boreal catchments; Geobiology -- Periodicals; Biogeochemistry -- Periodicals; Biotic communities -- Periodicals; Geophysics -- Periodicals; 577.14
• DOI: 10.1002/jgrg.20058
• Languages: English
• ISSNs: 2169-8953

Abstract

Abstract: [1] Boreal ecosystems represent a large carbon (C) reservoir and a substantial source of greenhouse gases. Hydrologic conditions dictate whether C leached from boreal soils is processed in catchments or flushed to less productive environments via the stream. This study quantified hydrologic and biogeochemical C loss from a boreal catchment underlain by frozen silt, where flowpaths may deepen as the active layer thaws over the summer. We hypothesized a decrease in the magnitude of C mineralization over the summer associated with changing flowpaths and decreasing hydrologic connectivity, organic matter lability, and nitrogen (N) availability. Conservative tracers were used to partition C and N loss between catchment export and biogeochemical processing. Coupling tracers with tributary and porewater chemistry indicated C and N cycling in soil flowpaths, with an exponential decrease over the summer. Nitrate was primarily reduced in hillslope flowpaths and the lack of N reaching the stream appeared to limit C mineralization. Stream export accounted for the greatest loss of C, removing 247 and 113 mol hr −1 in the early and late summer, respectively. Reactivity was related to hydrologic connectivity between the soils and stream, which was greatest early in the summer and following a large flood. While a warming climate may increase storage potential in thawed soils, the early‐season flush of labile material and late‐season runoff through mineral flowpaths may maintain high C export rates. Therefore, we highlight physical export as a dominant cause of aqueous C loss from silty catchments as the Arctic continues to thaw. Key Points: Changes in boreal runoff affect carbon and nitrogen transport and cycling Dissolved organic carbon export was greater than mineralization Nitrate was reduced on the hillslopes and in the stream, with only minor export