Sizable carbon emission from the floodplain of Ob River
The Ob River floodplain is the second largest floodplain in the world. Despite its vast area, estimates of carbon (C) emissions from the Ob River floodplain are largely absent. Here we present seasonal C emission and water area extent from the main channel and the floodplain along a ~4 km reach in t...
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ftdoajarticles:oai:doaj.org/article:10f3c3374da8481d951da67e81f674d7 2023-05-15T17:48:42+02:00 Sizable carbon emission from the floodplain of Ob River Ivan V. Krickov Svetlana Serikova Oleg S. Pokrovsky Sergey N. Vorobyev Artem G. Lim Matthias B. Siewert Jan Karlsson 2021-11-01T00:00:00Z https://doi.org/10.1016/j.ecolind.2021.108164 https://doaj.org/article/10f3c3374da8481d951da67e81f674d7 EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S1470160X21008293 https://doaj.org/toc/1470-160X 1470-160X doi:10.1016/j.ecolind.2021.108164 https://doaj.org/article/10f3c3374da8481d951da67e81f674d7 Ecological Indicators, Vol 131, Iss , Pp 108164- (2021) Floodplain Greenhouse gases Ob river Seasonal influences Carbon emission Ecology QH540-549.5 article 2021 ftdoajarticles https://doi.org/10.1016/j.ecolind.2021.108164 2022-12-31T09:22:05Z The Ob River floodplain is the second largest floodplain in the world. Despite its vast area, estimates of carbon (C) emissions from the Ob River floodplain are largely absent. Here we present seasonal C emission and water area extent from the main channel and the floodplain along a ~4 km reach in the boreal zone of the Ob River. We found strong seasonality in water area extent of the Ob main channel (~1.8 km2) and floodplain (~3 km2) with water covering 34% of land during flood and subsequently declining to ~16% and ~14% during summer and autumn baseflow, respectively. The C emissions also varied seasonally over the open water period, ranging from −0.1 to 0.6 g C m−2 d−1 for the Ob main channel and from 0 to 9 g C m−2 d−1 for the floodplain. The dissolved organic carbon positively affected CO2 concentrations and fluxes in the floodplain during all seasons, whereas pH and oxygen concentration negatively impacted CO2 concentrations and fluxes. Some nutrients (ammonia and phosphate) positively correlated with CO2 and CH4 concentrations in summer. The total C emission from the study reach (1.8 km2 main channel, 3 km2 floodplain) during moderate flooding was 236 ± 51 tons C yr−1 (>99% CO2, <1% CH4) with the floodplain accounting for ~65%. The contribution of the floodplain to the net river C evasion may be even greater during years of high flooding and in northern regions of the Ob River basin, where floodplain soils are more C-rich and are underlain by permafrost, and in years with more extensive flooding. Article in Journal/Newspaper ob river permafrost Directory of Open Access Journals: DOAJ Articles Ecological Indicators 131 108164 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Floodplain Greenhouse gases Ob river Seasonal influences Carbon emission Ecology QH540-549.5 |
spellingShingle |
Floodplain Greenhouse gases Ob river Seasonal influences Carbon emission Ecology QH540-549.5 Ivan V. Krickov Svetlana Serikova Oleg S. Pokrovsky Sergey N. Vorobyev Artem G. Lim Matthias B. Siewert Jan Karlsson Sizable carbon emission from the floodplain of Ob River |
topic_facet |
Floodplain Greenhouse gases Ob river Seasonal influences Carbon emission Ecology QH540-549.5 |
description |
The Ob River floodplain is the second largest floodplain in the world. Despite its vast area, estimates of carbon (C) emissions from the Ob River floodplain are largely absent. Here we present seasonal C emission and water area extent from the main channel and the floodplain along a ~4 km reach in the boreal zone of the Ob River. We found strong seasonality in water area extent of the Ob main channel (~1.8 km2) and floodplain (~3 km2) with water covering 34% of land during flood and subsequently declining to ~16% and ~14% during summer and autumn baseflow, respectively. The C emissions also varied seasonally over the open water period, ranging from −0.1 to 0.6 g C m−2 d−1 for the Ob main channel and from 0 to 9 g C m−2 d−1 for the floodplain. The dissolved organic carbon positively affected CO2 concentrations and fluxes in the floodplain during all seasons, whereas pH and oxygen concentration negatively impacted CO2 concentrations and fluxes. Some nutrients (ammonia and phosphate) positively correlated with CO2 and CH4 concentrations in summer. The total C emission from the study reach (1.8 km2 main channel, 3 km2 floodplain) during moderate flooding was 236 ± 51 tons C yr−1 (>99% CO2, <1% CH4) with the floodplain accounting for ~65%. The contribution of the floodplain to the net river C evasion may be even greater during years of high flooding and in northern regions of the Ob River basin, where floodplain soils are more C-rich and are underlain by permafrost, and in years with more extensive flooding. |
format |
Article in Journal/Newspaper |
author |
Ivan V. Krickov Svetlana Serikova Oleg S. Pokrovsky Sergey N. Vorobyev Artem G. Lim Matthias B. Siewert Jan Karlsson |
author_facet |
Ivan V. Krickov Svetlana Serikova Oleg S. Pokrovsky Sergey N. Vorobyev Artem G. Lim Matthias B. Siewert Jan Karlsson |
author_sort |
Ivan V. Krickov |
title |
Sizable carbon emission from the floodplain of Ob River |
title_short |
Sizable carbon emission from the floodplain of Ob River |
title_full |
Sizable carbon emission from the floodplain of Ob River |
title_fullStr |
Sizable carbon emission from the floodplain of Ob River |
title_full_unstemmed |
Sizable carbon emission from the floodplain of Ob River |
title_sort |
sizable carbon emission from the floodplain of ob river |
publisher |
Elsevier |
publishDate |
2021 |
url |
https://doi.org/10.1016/j.ecolind.2021.108164 https://doaj.org/article/10f3c3374da8481d951da67e81f674d7 |
genre |
ob river permafrost |
genre_facet |
ob river permafrost |
op_source |
Ecological Indicators, Vol 131, Iss , Pp 108164- (2021) |
op_relation |
http://www.sciencedirect.com/science/article/pii/S1470160X21008293 https://doaj.org/toc/1470-160X 1470-160X doi:10.1016/j.ecolind.2021.108164 https://doaj.org/article/10f3c3374da8481d951da67e81f674d7 |
op_doi |
https://doi.org/10.1016/j.ecolind.2021.108164 |
container_title |
Ecological Indicators |
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131 |
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108164 |
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