Linking Sediment Characteristics to Methane Emission Potential in Subarctic Lakes

Monday, 15 December 2014
Laura Ann Logozzo1, Apryl Lee Perry2, Martin Wik3, Brett F Thornton3, Patrick M Crill4, Joel E Johnson5 and Ruth K Varner6, (1)CUNY City College, New York, NY, United States, (2)University of New Hampshire Main Campus, Durham, NH, United States, (3)Stockholm University, Dept. of Geological Sciences, Stockholm, Sweden, (4)Stockholm University, Stockholm, Sweden, (5)University of New Hampshire, Dept. of Earth Sciences, Durham, NH, United States, (6)Univ New Hampshire, Durham, NH, United States
High latitudes are experiencing warmer average annual temperatures, resulting in the thawing of permafrost, and possibly, the increased emission of methane (CH4) from lakes and ponds. One potential impact of permafrost thaw is increased runoff of organic matter into streams, lakes and ponds. Warming can also potentially increase lake sediment temperatures, resulting in a lower methane (CH4) storage capacity and increased CH4 production. We focused our study on six lakes of varying size, location, and characteristics, located in the Stordalen Mire area in northernmost Sweden. We collected sediment cores in each lake and analyzed the dissolved CH4 in the sediment at various depths in the core. The sediment CH4 concentrations were compared to the grain sizes and compositions (total organic carbon (TOC), total sulfur (S), and total nitrogen) of the sediment at the corresponding depths. We also measured dissolved CH4 concentrations in the lake water and compared them to those of the sediment. We found that on average, the CH4 concentration was higher (16.7 μgCHgds-1 ± 16.4) in sediments with more TOC (31.4 wt % ± 10.8). There was also a strong positive correlation between sediment CH4 and total S (r2 = 0.37, p = 0.165), between sediment CH4 and TOC (r2 = 0.53, p = 0.101), and between TOC and total S (r2 = 0.64, p = 0.066). This indicates in situ production of CH in the lake sediment at depths of peak CH4 concentrations in at least two of the lakes. The peak of dissolved CH4 was located deeper in the cores although this depth varied among the lakes. In four lakes, we found high CH4 concentrations in the sediment, as well as high CH4 concentrations in the water, indicating little oxidation in the water column or persistent CH4 production in the sediment. This suggests that at least four of our studied lakes have great potential to release a substantial amount of their produced CH4 to the atmosphere.