The effect of urbanisation on wintertime soil respiration in the Russian Arctic

Purpose: With ongoing global warming, the carbon (C) balance of Arctic ecosystems has become a ‘hot’ topic; however, C stocks and fluxes in the soil of Arctic cities remain overlooked. The research aimed to estimate wintertime soil respiration and its contribution to the cumulative annual CO2 emission from urban and natural soil of Apatity town in the Russian Arctic zone. Materials and methods: Soil respiration and microclimatic parameters (i.e., air temperature, soil temperature at 0 cm, 7 cm and 20 cm, and snow height) were observed from November 2020 until May 2023 at two urban (UR) sites (UR1 was in the town centre, and UR2 was in the town’s outskirts) in comparison to the natural forested area. Soil chemical (i.e., bulk density, pHw, contents of available P, total C, N, bulk contents of Cu and Ni) and microbial (i.e., Cmic, BR, qCO2, number of rRNA gene copies and community-level physiological profile) properties were analysed to explain patterns in soil respiration. Results: A thicker snow layer and warmer soil temperature at the urban sites determined a higher than at the natural site cumulative annual soil CO2 efflux. The wintertime and snowy-period respiration accounted for 20% and 50% of the cumulative annual soil CO2 efflux, respectively, with remarkable spikes during the thawing period. The high variation in soil respiration between urban sites was explained by different states of microbial communities, with higher activity shown for younger and more intensively managed soil at the UR2 site. Conclusion: An adequate estimate of soil C balance in Arctic cities must consider the wintertime soil respiration as an essential part of the cumulative annual CO2 efflux, whereas monitoring points inside the cities represent the gradient in mesoclimatic conditions driven by the urban heat island effect as well as the age and management of urban soils. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024.

Авторы
Saltan N. , Vasenev V. , Korneykova M. , Slukovskaya M. , Zavodskikh M. , Sarzhanov D.
Язык
Английский
Статус
Опубликовано
Год
2024
Организации
  • 1 Polar Alpine Botanical Garden-Institute — Subdivision of the Federal Research Centre, Kola Science Centre of Russian Academy of Sciences, Apatity, Russian Federation
  • 2 Soil Geography and Landscape Group, Wageningen University, Wageningen, 6707, Netherlands
  • 3 Agrarian-Technological Institute, Peoples’ Friendship University of Russia (RUDN University), Moscow, Russian Federation
  • 4 Institute of North Industrial Ecology Problems Subdivision of the Federal Research Center, Kola Science Centre of Russian Academy of Science, Apatity, Russian Federation
  • 5 Laboratory of Nature-Inspired Technologies and Environmental Safety of the Arctic, Kola Science Centre, Russian Academy of Sciences, Apatity, Russian Federation
Ключевые слова
CO<sub>2</sub> emission; Freezing–thawing regimes; Microclimatic parameters; Polar region; Soil C balance
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