1 Aarhus University2 Department of Bioscience - Center for Geomicrobiology, Department of Bioscience, Science and Technology, Aarhus University3 University of Koblenz-Landau4 Eawag5 Nordisk Center for Jordens Udvikling (NordCEE)6 Federal Institute of Hydrology (BfG)7 RD2 Marine Biogeochemistry8 Department of Bioscience - Center for Geomicrobiology, Department of Bioscience, Science and Technology, Aarhus University
Inland waters transport and transform substantial amounts of carbon and account for similar to 18% of global methane emissions. Large reservoirs with higher areal methane release rates than natural waters contribute significantly to freshwater emissions. However, there are millions of small dams worldwide that receive and trap high loads of organic carbon and can therefore potentially emit significant amounts of methane to the atmosphere. We evaluated the effect of damming on methane emissions in a central European impounded river. Direct comparison of riverine and reservoir reaches, where sedimentation in the latter is increased due to trapping by dams, revealed that the reservoir reaches are the major source of methane emissions (similar to 0.23 mmol CH4 m(-2) d(-1) vs similar to 19.7 mmol CH4 m(-2) d(-1), respectively) and that areal emission rates far exceed previous estimates for temperate reservoirs or rivers. We show that sediment accumulation correlates with methane production and subsequent ebullitive release rates and may therefore be an excellent proxy for estimating methane emissions from small reservoirs. Our results suggest that sedimentation-driven methane emissions from dammed river hot spot sites can potentially increase global freshwater emissions by up to 7%.
Environmental Science and Technology (washington), 2013, Vol 47, Issue 15, p. 8130-8137