Wildfires trigger multi-decadal increases in sedimentation rate and metal loading to subarctic montane lakes

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dc.contributor.author
Pelletier, Nicolas
Chételat, John
Sinon, Sarah
Vermaire, Jesse C.
dc.date.accepted
2022-02-04
dc.date.accessioned
2024-08-28T18:08:53Z
dc.date.available
2024-08-28T18:08:53Z
dc.date.issued
2022-06-10
dc.date.submitted
2021-10-25
dc.description.abstract - en
We evaluated how two large wildfires affected the sedimentation rate and accumulation of lead (Pb), mercury (Hg), and cadmium (Cd) in sediment of four subarctic montane lakes in the Yukon, Canada. The wildfires occurred 60 and 20 years (1958, 1998) before sediment collection in 2018. Site-specific fire exposure was inferred from the charcoal accumulation histories in the lake sediments and the burned catchment area was determined from historical fire maps. The two major wildfires caused a two to five-fold increase in sedimentation rates and a two to eight-fold increase in sediment metal accumulation rates in Little Fox Lake. The mass accumulation rates of metals in Little Fox Lake sediment increased by a maximum of 2.7-4.7 mg Pb m<sup>-2</sup> yr<sup>-1</sup>, 19-29 μg Hg m<sup>-2</sup> yr<sup>-1</sup> and 37-114 μg Cd m<sup>-2</sup> yr<sup>-1</sup> following wildfires. Modelling using elemental ratios of lithogenic sources suggested a large proportion of the Pb and Hg accumulating in post-fire sediment was from remobilized legacy anthropogenic pollution. In contrast, Cd fluxes were consistent with variation in catchment weathering. Impacts of wildfires were visible but more muted in the sediment of Little Braeburn Lake, whereas Fox Lake and Grayling Lake sediments showed little to no wildfire impact and served as a reference for external (long-range) metal deposition. Major changes to lake sediment geochemistry in Little Fox Lake were caused by the lack of vegetation and soil recovery in the catchment following the severe 1998 fire. Wildfire impacts were persistent in the lake more than 20 years after the last fire, with no sign of a return to pre-fire Pb, Hg, and Cd accumulation rates. This study shows that wildfires in northern montane catchments can significantly increase the rate of metal accumulation in affected lakes, thereby impeding recovery from reductions in anthropogenic air emissions of these metals.
dc.identifier.issn
1879-1026
0048-9697
dc.identifier.uri
https://open-science.canada.ca/handle/123456789/2893
dc.language.iso
en
dc.publisher
Elsevier
dc.relation.isreplacedby
https://doi.org/10.1016/j.scitotenv.2022.153738
dc.rights - en
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
dc.rights - fr
Creative Commons Attribution - Pas d'utilisation commerciale - Pas de modification 4.0 International (CC BY-NC-ND 4.0)
dc.rights.openaccesslevel - en
Green
dc.rights.openaccesslevel - fr
Vert
dc.rights.uri - en
https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.rights.uri - fr
https://creativecommons.org/licenses/by-nc-nd/4.0/deed.fr
dc.subject - en
Nature and environment
Science and technology
dc.subject - fr
Nature et environnement
Sciences et technologie
dc.subject.en - en
Nature and environment
Science and technology
dc.subject.fr - fr
Nature et environnement
Sciences et technologie
dc.title - en
Wildfires trigger multi-decadal increases in sedimentation rate and metal loading to subarctic montane lakes
dc.type - en
Accepted manuscript
dc.type - fr
Manuscrit accepté
local.acceptedmanuscript.articlenum
153738
local.article.journaltitle
Science of The Total Environment
local.article.journalvolume
824
local.pagination
42 pages
local.peerreview - en
Yes
local.peerreview - fr
Oui
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