Responses of N2O emissions to spring thaw period in a typical continuous permafrost region of the Daxing'an Mountains, northeast China

Abstract In the context of global climate warming, spring thaw period had been changed in the permafrost regions, which significantly affect heat and water dynamics, along with soil microbial community structure and diversity, and microbially-mediated nitrogen cycle changes. However, in - situ N 2 O emission research is scarce in the permafrost regions and the drivers of N 2 O emission during spring thaw period remain unclear. We selected three type of swamp forests in the permafrost region to investigate the N 2 O emissions during spring thaw period from 17 March to 23 May 2017. We found that N 2 O emission ranged from −35.75 to 74.17 μg m −2  h −1 in the permafrost region during spring thaw period, and there was no significant large burst of N 2 O emissions as observed in other ecosystems. The N 2 O emission during spring thaw period were lower than those from growing season, which were significant affected by soil temperature. During spring thaw period, swamp forest types had no significantly influence on N 2 O emissions, which mainly limited by NO 3 − -N content. Stepwise multiple linear regression indicated that the air temperature, thawing depth, soil temperature, soil moisture, pH, NH 4 + -N, NO 3 − -N, TOC, TN, and C/N ratio were the environmental factors which significant effecting the N 2 O emissions. In the field campaign, cumulative N 2 O emissions were mainly controlled by thawing depth, soil moisture, pH, NH 4 + -N, NO 3 − -N and TN during spring thaw period. Overall, the results demonstrate that in the permafrost ecosystems spring thaw period is an important source of N 2 O emissions.