DOI: 10.1111/gcb.12607
论文题名: Permafrost conditions in peatlands regulate magnitude, timing, and chemical composition of catchment dissolved organic carbon export
作者: Olefeldt D. ; Roulet N.T.
刊名: Global Change Biology
ISSN: 13541013
出版年: 2014
卷: 20, 期: 10 起始页码: 3122
结束页码: 3136
语种: 英语
英文关键词: DOC
; Fen
; Hydrograph separation
; Palsa
; Permafrost plateau
; Subarctic
; SUVA
; Wetlands
Scopus关键词: carbon cycle
; catchment
; chemical composition
; dissolved organic carbon
; fen
; hydrograph
; organic soil
; palsa
; peatland
; permafrost
; carbon
; ground water
; soil
; carbon cycle
; chemistry
; climate
; permafrost
; season
; soil
; Sweden
; water flow
; wetland
; Carbon
; Carbon Cycle
; Climate
; Groundwater
; Permafrost
; Seasons
; Soil
; Sweden
; Water Movements
; Wetlands
英文摘要: Permafrost thaw in peatlands has the potential to alter catchment export of dissolved organic carbon (DOC) and thus influence downstream aquatic C cycling. Subarctic peatlands are often mosaics of different peatland types, where permafrost conditions regulate the hydrological setting of each type. We show that hydrological setting is key to observed differences in magnitude, timing, and chemical composition of DOC export between permafrost and nonpermafrost peatland types, and that these differences influence the export of DOC of larger catchments even when peatlands are minor catchment components. In many aspects, DOC export from a studied peatland permafrost plateau was similar to that of a forested upland catchment. Similarities included low annual export (2-3 g C m-2) dominated by the snow melt period (~70%), and how substantial DOC export following storms required wet antecedent conditions. Conversely, nonpermafrost fens had higher DOC export (7 g C m-2), resulting from sustained hydrological connectivity during summer. Chemical composition of catchment DOC export arose from the mixing of highly aromatic DOC from organic soils from permafrost plateau soil water and upland forest surface horizons with nonaromatic DOC from mineral soil groundwater, but was further modulated by fens. Increasing aromaticity from fen inflow to outlet was substantial and depended on both water residence time and water temperature. The role of fens as catchment biogeochemical hotspots was further emphasized by their capacity for sulfate retention. As a result of fen characteristics, a 4% fen cover in a mixed catchment was responsible for 34% higher DOC export, 50% higher DOC concentrations and ~10% higher DOC aromaticity at the catchment outlet during summer compared to a nonpeatland upland catchment. Expansion of fens due to thaw thus has potential to influence landscape C cycling by increasing fen capacity to act as biogeochemical hotspots, amplifying aquatic C cycling, and increasing catchment DOC export. © 2014 John Wiley & Sons Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/62227
Appears in Collections: 影响、适应和脆弱性
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作者单位: Department of Geography, McGill University, 805 Sherbrooke St W, Montreal, QC, Canada; Global Enviromental and Climate Change Research Centre, McGill University, Montreal, QC, Canada; Department of Integrative Biology, University of Guelph, Guelph, ON, Canada
Recommended Citation:
Olefeldt D.,Roulet N.T.. Permafrost conditions in peatlands regulate magnitude, timing, and chemical composition of catchment dissolved organic carbon export[J]. Global Change Biology,2014-01-01,20(10)