Fine-Scale Assessment of Greenhouse Gases Fluxes from a Boreal Peatland Pond
Ponds are abundant in the boreal peatland landscape, which are potential hotspots for greenhouse gas (GHG) emissions. However, compared to large lakes, ponds are difficult to identify by satellite, and they have not been adequately studied. Here, we observed methane (CH 4 ), carbon dioxide (CO 2 ),...
| Published in: | Water |
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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
MDPI AG
2023
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| Subjects: | |
| Online Access: | https://doi.org/10.3390/w15020307 https://doaj.org/article/2fb34171bcf14d95a8b6fa472ac42a88 |
| Summary: | Ponds are abundant in the boreal peatland landscape, which are potential hotspots for greenhouse gas (GHG) emissions. However, compared to large lakes, ponds are difficult to identify by satellite, and they have not been adequately studied. Here, we observed methane (CH 4 ), carbon dioxide (CO 2 ), and nitrous oxide (N 2 O) fluxes in the growing season at three sites along the water table gradient from the pelagic zone, littoral zone and bog across a shallow pond in a boreal peatland landscape in Northeastern China. The results showed that the littoral zone, dominated by herb Carex, was the hotspot for CH 4 emissions. CH 4 fluxes in littoral zone averaged 78.98 ± 19.00 mg m −2 h −1 . The adjacent bog was a weak source of CH 4 emissions, with an average flux of 0.07 ± 0.05 mg m −2 h −1 . Within the pond, CH 4 was mainly emitted through ebullition, accounting for 88.56% of the total CH 4 fluxes, and the ebullition fluxes were negatively correlated with dissolved oxygen (DO). CO 2 fluxes were highest in the pelagic zone, with an average of 419.76 ± 47.25 mg m −2 h −1 . Wind and strong sediment respiration were key factors that led to the high fluxes. The observed three sites were all atmospheric N 2 O sinks ranging from −0.92 to −10.90 μg m −2 h −1 . This study highlights the spatial variation in greenhouse gas fluxes from the pond and its adjacent bog, ignoring the ecotone area may underestimate CH 4 fluxes. Although ponds are a hotspot for CH 4 and CO 2 emissions, they can also be a sink for N 2 O, which provides a reference for the quantification of global pond GHG fluxes. Therefore, finer-scale in situ observations are necessary to better understand the feedback of permafrost peatland ponds to global warming. |
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