Redox dynamics in the active layer of an Arctic headwater catchment; examining the potential for transfer of dissolved methane from soils to stream water

Lorna E. Street*, Joshua F. Dean, Michael F. Billett, Robert Baxter, Kerry J. Dinsmore, Jason S. Lessels, Jens Arne Subke, Doerthe Tetzlaff, Philip A. Wookey

*Corresponding author for this work

Research output: Contribution to journalArticle

9 Citations (Scopus)
4 Downloads (Pure)

Abstract

The linkages between methane production, transport, and release from terrestrial and aquatic systems are not well understood, complicating the task of predicting methane emissions. We present novel data examining the potential for the saturated zone of active layer soils to act as a source of dissolved methane to the aquatic system, via soil water discharge, within a headwater catchment of the continuous permafrost zone in Northern Canada. We monitored redox conditions and soil methane concentrations across a transect of soil profiles from midstream to hillslope and compare temporal patterns in methane concentrations in soils to those in the stream. We show that redox conditions in active layer soils become more negative as the thaw season progresses, providing conditions suitable for net methanogenesis and that redox conditions are sensitive to increased precipitation during a storm event-but only in shallower surface soil layers. While we demonstrate that methane concentrations at depth in the hillslope soils increase over the course of the growing season as reducing conditions develop, we find no evidence that this has an influence on stream water methane concentrations. Sediments directly beneath the stream bed, however, remain strongly reducing at depth throughout the thaw season and contain methane at concentrations 5 orders of magnitude greater than those in hillslope soils. The extent of substreambed methane sources, and the rates of methane transport from these zones, may therefore be important factors determining headwater stream methane concentrations under changing Arctic hydrologic regimes.

Original languageEnglish
Pages (from-to)2776-2792
Number of pages17
JournalJournal of geophysical research-Biogeosciences
Volume121
Issue number11
Early online date5 Nov 2016
DOIs
Publication statusPublished - Nov 2016

Fingerprint

active layer
Methane
headwater
Catchments
methane
Arctic region
soils
catchment
Soils
Water
water
soil
redox conditions
hillslope
methane production
Oxidation-Reduction
soil surface layers
permafrost
Permafrost
stream bed

Keywords

  • Hydrological processes
  • Hyporheic zone
  • Methanogenesis
  • Permafrost
  • Riparian
  • Trail Valley Creek

ASJC Scopus subject areas

  • Geophysics
  • Oceanography
  • Forestry
  • Ecology
  • Aquatic Science
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Redox dynamics in the active layer of an Arctic headwater catchment; examining the potential for transfer of dissolved methane from soils to stream water. / Street, Lorna E.; Dean, Joshua F.; Billett, Michael F.; Baxter, Robert; Dinsmore, Kerry J.; Lessels, Jason S.; Subke, Jens Arne; Tetzlaff, Doerthe; Wookey, Philip A.

In: Journal of geophysical research-Biogeosciences, Vol. 121, No. 11, 11.2016, p. 2776-2792.

Research output: Contribution to journalArticle

Street, Lorna E. ; Dean, Joshua F. ; Billett, Michael F. ; Baxter, Robert ; Dinsmore, Kerry J. ; Lessels, Jason S. ; Subke, Jens Arne ; Tetzlaff, Doerthe ; Wookey, Philip A. / Redox dynamics in the active layer of an Arctic headwater catchment; examining the potential for transfer of dissolved methane from soils to stream water. In: Journal of geophysical research-Biogeosciences. 2016 ; Vol. 121, No. 11. pp. 2776-2792.
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AU - Lessels, Jason S.

AU - Subke, Jens Arne

AU - Tetzlaff, Doerthe

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