B21H-0580
Greenhouse Gas Fluxes from Peatland Pools

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Ed Turner1, Andrew J Baird1, Michael F Billett2, Pippa J Chapman1, Kerry Jane Dinsmore3 and Joseph Holden4, (1)University of Leeds, School of Geography, Leeds, United Kingdom, (2)University of Stirling, Stirling, United Kingdom, (3)Centre for Ecology and Hydrology, Biosphere-Atmosphere Interactions, Edinburgh, United Kingdom, (4)University of Leeds, Leeds, United Kingdom
Abstract:
Peatlands contain around one third of the global soil carbon (C) stock. Understanding the processes in peatland C cycling, and in particular those involved in the release of the greenhouse gases (GHGs) CO2 and CH4 to the atmosphere, is a current research priority. Natural open-water pools are a common feature of many peatlands, and previous research suggests pools can be strong sources of atmospheric GHGs, particularly CH4, and thus have the potential to play an important role in global radiative forcing. The area of open-water in peatlands is rapidly expanding in a warming Arctic (e.g. Walter et al., 2007) while artificially created pools are becoming more commonplace in the recent drive to restore the hydrological functioning of drained peatlands by blocking ditches.

We present the results of >2 years of comprehensive field monitoring from pool complexes in the Flow Country of northern Scotland, the largest expanse (c.4000 km2) of blanket bog in Europe. Concentrations and fluxes of CO2 and CH4 are presented from 12 intensively monitored pools and the adjacent terrestrial surface. We examined both natural (n = 6) and artificial (n = 6) pools, which allowed us to quantify how pools created during restoration compare to undisturbed sites. C and hydrology budgets were determined for the study pools and the adjacent terrestrial surface. Dissolved concentrations of GHGs ranged from 0.08−4.68 mg CO2-C L-1 and 0.01−731 µg CH4-C L-1 in natural pools, and 0.29−10.38 mg CO2-C L-1 and 0.04−239 µg CH4-C L-1 in artificial pools. GHG fluxes from natural pool surfaces ranged between -2.47−653 mg CH4 m-2 d-1 and -31.7−14.8 g CO2 m-2 d-1. Artificial pool GHG fluxes were -8.19−581 mg CH4 m-2 d-1 and -7.66−34.9 g CO2 m-2 d-1. We provide more accurate GHG budgets for peatlands with natural pool complexes by considering their relative importance at the landscape-scale, and outline the potential effect on GHG fluxes when creating artificial pools during peatland restoration activities.

WALTER, K. M., SMITH, L. C. & CHAPIN, F. S. 2007. Methane bubbling from northern lakes: present and future contributions to the global methane budget. Philosophical Transactions of the Royal Society A, 365, 1657-1676.