2022
DOI: 10.1007/s00284-021-02690-8
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Nitrous Oxide Emission in Response to pH from Degrading Palsa Mire Peat Due to Permafrost Thawing

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Cited by 3 publications
(2 citation statements)
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“…SC-H2 was small, but N 2 O could be accumulated. However, the palsa mounds are formed due to the ice core under the Sphagnum peat layer in the subarctic climate, and once they collapse after permafrost thawing, the peat acidity will be neutralized to some extent by mixing with mineral material and minerogenic water flow (Seppälä, 2011 ; Takatsu et al, 2022 ).…”
Section: Discussionmentioning
confidence: 99%
“…SC-H2 was small, but N 2 O could be accumulated. However, the palsa mounds are formed due to the ice core under the Sphagnum peat layer in the subarctic climate, and once they collapse after permafrost thawing, the peat acidity will be neutralized to some extent by mixing with mineral material and minerogenic water flow (Seppälä, 2011 ; Takatsu et al, 2022 ).…”
Section: Discussionmentioning
confidence: 99%
“…Peatland ponds with thermokarst expansion often emit large amounts of CH 4 and have net emissions of CO 2 (Elder et al., 2021; Walter Anthony et al., 2018), while the effects on pond N 2 O fluxes are unknown. Studies of boreal peatland N 2 O fluxes in permafrost regions come primarily from northern Europe and have shown generally low N 2 O emissions from intact peat plateaus and palsas, but at times very high emissions during initial stages of permafrost thaw and soil warming associated with increased availability of inorganic N and increases in pH (Takatsu et al., 2022; Voigt, Lamprecht, et al., 2017). Thermokarst wetlands with mineral soils have in some regions led to high N 2 O emissions (Abbott & Jones, 2015; Marushchak et al., 2021; Yang et al., 2018), but N 2 O emissions did not increase with the development of Tibetan thermokarst bogs (Sun et al., 2021).…”
Section: Introductionmentioning
confidence: 99%