Dynamics of Dissolved Inorganic Carbon and CO <sub>2</sub> Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River

Аннотация

Abstract: The results of studying the dynamics of parameters of the carbonate system in the middle and lower reaches of the Ob River in July 2016 were analyzed. The distributions of the carbonate characteristics of the river waters were found to follow a steady latitudinal trend determined by the landscape-geochemical conditions of the drainage basin and by the permafrost distribution. The first field data on the magnitude and direction of the CO ₂ fluxes in the Ob River water–atmosphere system were presented. It was shown that the waters in the middle and lower reaches of the river are multiply supersaturated with CO ₂ with respect to its atmospheric content, and the daily average evasion reaches 625.9 mmol m ^–2 day ^–1 at an average value of 102.1 mmol m ^–2 day ^–1 . It was determined that the waters of the Ob River in the studied reaches are a significant CO ₂ source to the atmosphere; according to conservative estimates, the total flux in July was 2 × 10 ¹¹ g of carbon in the form of CO ₂ .

Язык оригинала	Английский
Страницы (с-по)	52-57
Число страниц	6
Журнал	Doklady Chemistry
Том	484
Номер выпуска	2
DOI	https://doi.org/10.1134/S0012500819020101
Состояние	Опубликовано - 1 авг 2019

ASJC Scopus subject areas

Chemistry(all)

Доступ к документу

10.1134/S0012500819020101

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Pipko, I. I., Pugach, S. P., Savichev, O. G., Repina, I. A., Shakhova, N. E., Moiseeva, Y. A., Barskov, K. V., Sergienko, V. I., & Semiletov, I. P. (2019). Dynamics of Dissolved Inorganic Carbon and CO ₂ Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River. Doklady Chemistry, 484(2), 52-57. https://doi.org/10.1134/S0012500819020101

Dynamics of Dissolved Inorganic Carbon and CO ₂ Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River. / Pipko, I. I.; Pugach, S. P.; Savichev, O. G.; Repina, I. A.; Shakhova, N. E.; Moiseeva, Yu A.; Barskov, K. V.; Sergienko, V. I.; Semiletov, I. P.

В: Doklady Chemistry, Том 484, № 2, 01.08.2019, стр. 52-57.

Результат исследований: Материалы для журнала › Статья › рецензирование

Pipko, II, Pugach, SP, Savichev, OG, Repina, IA, Shakhova, NE, Moiseeva, YA, Barskov, KV, Sergienko, VI & Semiletov, IP 2019, 'Dynamics of Dissolved Inorganic Carbon and CO ₂ Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River', Doklady Chemistry, том. 484, № 2, стр. 52-57. https://doi.org/10.1134/S0012500819020101

Pipko II, Pugach SP, Savichev OG, Repina IA, Shakhova NE, Moiseeva YA и соавт. Dynamics of Dissolved Inorganic Carbon and CO ₂ Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River. Doklady Chemistry. 2019 Авг. 1;484(2):52-57. https://doi.org/10.1134/S0012500819020101

Pipko, I. I. ; Pugach, S. P. ; Savichev, O. G. ; Repina, I. A. ; Shakhova, N. E. ; Moiseeva, Yu A. ; Barskov, K. V. ; Sergienko, V. I. ; Semiletov, I. P. / Dynamics of Dissolved Inorganic Carbon and CO ₂ Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River. В: Doklady Chemistry. 2019 ; Том 484, № 2. стр. 52-57.

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title = "Dynamics of Dissolved Inorganic Carbon and CO 2 Fluxes between the Water and the Atmosphere in the Main Channel of the Ob River",

abstract = " Abstract: The results of studying the dynamics of parameters of the carbonate system in the middle and lower reaches of the Ob River in July 2016 were analyzed. The distributions of the carbonate characteristics of the river waters were found to follow a steady latitudinal trend determined by the landscape-geochemical conditions of the drainage basin and by the permafrost distribution. The first field data on the magnitude and direction of the CO 2 fluxes in the Ob River water–atmosphere system were presented. It was shown that the waters in the middle and lower reaches of the river are multiply supersaturated with CO 2 with respect to its atmospheric content, and the daily average evasion reaches 625.9 mmol m –2 day –1 at an average value of 102.1 mmol m –2 day –1 . It was determined that the waters of the Ob River in the studied reaches are a significant CO 2 source to the atmosphere; according to conservative estimates, the total flux in July was 2 × 10 11 g of carbon in the form of CO 2 . ",

author = "Pipko, {I. I.} and Pugach, {S. P.} and Savichev, {O. G.} and Repina, {I. A.} and Shakhova, {N. E.} and Moiseeva, {Yu A.} and Barskov, {K. V.} and Sergienko, {V. I.} and Semiletov, {I. P.}",

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AU - Pipko, I. I.

AU - Pugach, S. P.

AU - Savichev, O. G.

AU - Repina, I. A.

AU - Shakhova, N. E.

AU - Moiseeva, Yu A.

AU - Barskov, K. V.

AU - Sergienko, V. I.

AU - Semiletov, I. P.

PY - 2019/8/1

Y1 - 2019/8/1

N2 - Abstract: The results of studying the dynamics of parameters of the carbonate system in the middle and lower reaches of the Ob River in July 2016 were analyzed. The distributions of the carbonate characteristics of the river waters were found to follow a steady latitudinal trend determined by the landscape-geochemical conditions of the drainage basin and by the permafrost distribution. The first field data on the magnitude and direction of the CO 2 fluxes in the Ob River water–atmosphere system were presented. It was shown that the waters in the middle and lower reaches of the river are multiply supersaturated with CO 2 with respect to its atmospheric content, and the daily average evasion reaches 625.9 mmol m –2 day –1 at an average value of 102.1 mmol m –2 day –1 . It was determined that the waters of the Ob River in the studied reaches are a significant CO 2 source to the atmosphere; according to conservative estimates, the total flux in July was 2 × 10 11 g of carbon in the form of CO 2 .

AB - Abstract: The results of studying the dynamics of parameters of the carbonate system in the middle and lower reaches of the Ob River in July 2016 were analyzed. The distributions of the carbonate characteristics of the river waters were found to follow a steady latitudinal trend determined by the landscape-geochemical conditions of the drainage basin and by the permafrost distribution. The first field data on the magnitude and direction of the CO 2 fluxes in the Ob River water–atmosphere system were presented. It was shown that the waters in the middle and lower reaches of the river are multiply supersaturated with CO 2 with respect to its atmospheric content, and the daily average evasion reaches 625.9 mmol m –2 day –1 at an average value of 102.1 mmol m –2 day –1 . It was determined that the waters of the Ob River in the studied reaches are a significant CO 2 source to the atmosphere; according to conservative estimates, the total flux in July was 2 × 10 11 g of carbon in the form of CO 2 .

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