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Minor methane emissions from an Alpine hydropower reservoir based on monitoring of diel and seasonal variability.

Authors :
Sollberger S
Wehrli B
Schubert CJ
DelSontro T
Eugster W
Source :
Environmental science. Processes & impacts [Environ Sci Process Impacts] 2017 Oct 18; Vol. 19 (10), pp. 1278-1291.
Publication Year :
2017

Abstract

We monitored CH <subscript>4</subscript> emissions during the ice-free period of an Alpine hydropower reservoir in the Swiss Alps, Lake Klöntal, to investigate mechanisms responsible for CH <subscript>4</subscript> variability and to estimate overall emissions to the atmosphere. A floating eddy-covariance platform yielded total CH <subscript>4</subscript> and CO <subscript>2</subscript> emission rates at high temporal resolution, while hydroacoustic surveys provided no indication of CH <subscript>4</subscript> ebullition. Higher CH <subscript>4</subscript> fluxes (2.9 ± 0.1 mg CH <subscript>4</subscript> per m <superscript>2</superscript> per day) occurred during the day when surface water temperatures were warmer and wind speeds higher than at night. Piston velocity estimates (k <subscript>600</subscript> ) showed an upper limit at high wind speeds that may be more generally valid also for other lakes and reservoirs with limited CH <subscript>4</subscript> dissolved in the water body: above 2.0 m s <superscript>-1</superscript> a further increase in wind speed did not lead to higher CH <subscript>4</subscript> fluxes, because under such conditions it is not the turbulent mixing and transport that limits effluxes, but the resupply of CH <subscript>4</subscript> to the lake surface. Increasing CH <subscript>4</subscript> fluxes during the warm season showed a clear spatial gradient once the reservoir started to fill up and flood additional surface area. The warm period contributed 27% of the total CH <subscript>4</subscript> emissions (2.6 t CH <subscript>4</subscript> per year) estimated for the full year and CH <subscript>4</subscript> accounted for 63% of carbonic greenhouse gas emissions. Overall, the average CH <subscript>4</subscript> emissions (1.7 to 2.2 mg CH <subscript>4</subscript> per m <superscript>2</superscript> per day determined independently from surface water samplings and eddy covariance, respectively) were small compared to most tropical and some temperate reservoirs. The resulting greenhouse gas (GHG) emissions in CO <subscript>2</subscript> -equivalents revealed that electricity produced in the Lake Klöntal power plant was relatively climate-friendly with a low GHG-to-power output ratio of 1.24 kg CO <subscript>2,eq</subscript> per MW h compared to 6.5 and 8.1 kg CO <subscript>2,eq</subscript> per MW h associated with the operation of solar photovoltaics and wind energy, respectively, or about 980 kg CO <subscript>2,eq</subscript> per MW h for coal-fired power plants.

Details

Language :
English
ISSN :
2050-7895
Volume :
19
Issue :
10
Database :
MEDLINE
Journal :
Environmental science. Processes & impacts
Publication Type :
Academic Journal
Accession number :
28840207
Full Text :
https://doi.org/10.1039/c7em00232g