Preprints
https://doi.org/10.5194/egusphere-2025-1111
https://doi.org/10.5194/egusphere-2025-1111
03 Apr 2025
 | 03 Apr 2025
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Ecosystem-scale greenhouse gas fluxes from actively extracted peatlands: water table depth drives interannual variability

Miranda Louise Hunter, Ian Strachan, Paul Moore, Sara Knox, and Maria Strack

Abstract. Peat extraction substantially alters a peatland’s surface-atmosphere exchange of carbon (C). The sites are drained, their vegetation is removed, and then the peat is vacuum harvested for use as a horticultural growing medium. Despite this disturbance covering only a small percentage of Canadian peatlands, the shift from being a net sink to a net source of C during the typical 15–40 plus years of active extraction makes it an important system to study. Ours is the first study in Canada to conduct ecosystem scale measurements of carbon dioxide (CO2) and methane (CH4) exchange using eddy covariance from actively extracted peatlands. In order to understand environmental drivers of seasonal and interannual patterns of CO2, and seasonal patterns of CH4 fluxes, daytime ecosystem scale measurements of CO2 and CH4, along with average hourly water table depth (WTD) and soil temperature, were conducted from March to October in 2020, 2021 and 2022 at a Western Site (near Drayton Valley, Alberta), and from May to October in 2020 and 2022 at an Eastern Site (near Rivière-du-Loup, Quebec). In contrast to the positive linear relationship observed in my studies, we observed a unimodal CO2 – WTD relationship, with fluxes peaking at WTDs of 47 cm. Water table depth drove interannual variability, suggesting that in deeply drained peatlands, we must consider that insufficient surface moisture conditions can reduce soil respiration. Soil temperature had a significant interaction with WTD with positive relationships during moderate and wet periods (WTD < 50 cm) and weakly positive to negative relationships during dry periods (WTD > 50 cm) with lower explanatory power. Thus, process-based models using soil temperature alone may overestimate fluxes from drained peatlands during dry periods. The sites were small sources of CH4 compared to natural boreal bogs, though we were not able to capture freeze-thaw periods. After making assumptions for missing nighttime and wintertime data, we estimated an annual CO2-C of 112 to 174 g C m-2 yr-1, which is considerably lower than Canada’s current Tier 2 emission factor. This research will aid in updating emission factors for peat extraction in Canada, and will help guide industry site management practices.

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Miranda Louise Hunter, Ian Strachan, Paul Moore, Sara Knox, and Maria Strack

Status: open (until 30 May 2025)

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Miranda Louise Hunter, Ian Strachan, Paul Moore, Sara Knox, and Maria Strack
Miranda Louise Hunter, Ian Strachan, Paul Moore, Sara Knox, and Maria Strack

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Short summary
Peatlands are a globally important land cover due to their role as a carbon sink, though peat extraction for horticultural use converts them to net sources. Through ecosystem scale measurements at peat extraction sites, this study found that carbon dioxide interannual variability is driven by water table position. A unimodal carbon dioxide-water table relationship suggests that maintaining dry conditions could be a management strategy to reduce carbon loss during the 30 plus years of extraction.
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