Pond greenhouse gas emissions controlled by duckweed coverage
Joseph S. Rabaey, James B. Cotner
Abstract
Freshwaters are significant contributors of greenhouse gases to the atmosphere, including carbon dioxide (CO 2 ), methane (CH 4 ), and nitrous oxide (N 2 O). Small waterbodies such as ponds are now recognized to have disproportionate greenhouse gas emissions relative to their size, but measured emissions from ponds have varied by several orders of magnitude. To assess drivers of variation in pond greenhouse gas dynamics, we measured concentrations and emissions of CO 2 , CH 4 , and N 2 O across 26 ponds in Minnesota, United States, during the ice-free season. The studied ponds differed in land-use, from urban stormwater ponds to natural forested ponds. The ponds were all sources of greenhouse gases, driven by large CH 4 emissions (mean 704 [sd 840] mg CH 4 -C m −2 d −1 ). CO 2 fluxes were variable, but on average a sink (mean −25.9 [sd 862] mg CO 2 -C m −2 d −1 ), and N 2 O emissions were generally low (mean 0.398 [sd 0.747] mg N 2 O-N m −2 d −1 ). Duckweed coverage on the water surfaces ranged from 0% to 100% coverage, and had the largest influence on water chemistry and greenhouse gas dynamics across the ponds. Duckweed covered ponds (ponds with greater than 85% coverage) had higher phosphorus levels and increased anoxia compared to ponds without duckweed (ponds with less than 12% coverage), leading to higher CH 4 concentrations and overall greenhouse gas emissions in the duckweed ponds. Duckweed ponds had a mean emission rate in CO 2 equivalents of 30.9 g C m −2 d −1 compared to 11.0 g C m −2 d −1 in non-duckweed ponds.