Carbonate system of the Razdolnaya River estuary (Amur Bay, Sea of Japan)

Abstract

Two methods, the total alkalinity measurement by Bruevich [4] and pH measurement in a cell without liquid junction [11], were suggested for study of the carbonate system of estuaries. Based on new measurements, the empirical equations were obtained for the first and second seawater concentration constants of carbonic acid for the ranges of salinity 0-40‰ and temperatures 0-30°C. Applying the constants and above methods, we studied the carbonate system of the Razdol'naya River-Amur Bay estuary in two expeditions of July 2001, the first in a period of average water level and the second after a flood. In the latter survey, extremely low values (∼60 μatm) of pCO₂ (carbon dioxide partial pressure) were recorded in the seaward part of the estuary and extremely high (∼13300 μatm) were noted in the river. High pCO₂ in the surface water was caused by intense bacterial activity, and low levels were caused by phytoplankton bloom. The nonconservative behavior of the total alkalinity and dissolved inorganic carbon was revealed in the estuary. Based on the data of the carbonate system, the production/destruction of organic matter was assessed.

Original language	English
Pages (from-to)	43-52
Number of pages	10
Journal	Russian Journal of Marine Biology
Volume	31
Issue number	1
DOIs	https://doi.org/10.1007/s11179-005-0042-5
Publication status	Published - Jan 2005
Externally published	Yes

Keywords

Carbonate system
Estuary
Primary production

ASJC Scopus subject areas

Oceanography
Aquatic Science

Access to Document

10.1007/s11179-005-0042-5

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Tishchenko, P. Y., Wong, C. S., Volkova, T. I., Gramm-Osipov, L. M., Johnson, V. K., Dudarev, O. V., Zvalinskii, V. I., Nedashkovskii, A. P., Pavlova, G. Y., Chichkin, R. V., Sagalaev, S. G., Shevtsova, O. V., & Shkirnikova, E. M. (2005). Carbonate system of the Razdolnaya River estuary (Amur Bay, Sea of Japan). Russian Journal of Marine Biology, 31(1), 43-52. https://doi.org/10.1007/s11179-005-0042-5

Carbonate system of the Razdolnaya River estuary (Amur Bay, Sea of Japan). / Tishchenko, P. Ya; Wong, C. S.; Volkova, T. I.; Gramm-Osipov, L. M.; Johnson, V. K.; Dudarev, O. V.; Zvalinskii, V. I.; Nedashkovskii, A. P.; Pavlova, G. Yu; Chichkin, R. V.; Sagalaev, S. G.; Shevtsova, O. V.; Shkirnikova, E. M.

In: Russian Journal of Marine Biology, Vol. 31, No. 1, 01.2005, p. 43-52.

Research output: Contribution to journal › Article › peer-review

Tishchenko, PY, Wong, CS, Volkova, TI, Gramm-Osipov, LM, Johnson, VK, Dudarev, OV, Zvalinskii, VI, Nedashkovskii, AP, Pavlova, GY, Chichkin, RV, Sagalaev, SG, Shevtsova, OV & Shkirnikova, EM 2005, 'Carbonate system of the Razdolnaya River estuary (Amur Bay, Sea of Japan)', Russian Journal of Marine Biology, vol. 31, no. 1, pp. 43-52. https://doi.org/10.1007/s11179-005-0042-5

Tishchenko, P. Ya ; Wong, C. S. ; Volkova, T. I. ; Gramm-Osipov, L. M. ; Johnson, V. K. ; Dudarev, O. V. ; Zvalinskii, V. I. ; Nedashkovskii, A. P. ; Pavlova, G. Yu ; Chichkin, R. V. ; Sagalaev, S. G. ; Shevtsova, O. V. ; Shkirnikova, E. M. / Carbonate system of the Razdolnaya River estuary (Amur Bay, Sea of Japan). In: Russian Journal of Marine Biology. 2005 ; Vol. 31, No. 1. pp. 43-52.

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abstract = "Two methods, the total alkalinity measurement by Bruevich [4] and pH measurement in a cell without liquid junction [11], were suggested for study of the carbonate system of estuaries. Based on new measurements, the empirical equations were obtained for the first and second seawater concentration constants of carbonic acid for the ranges of salinity 0-40‰ and temperatures 0-30°C. Applying the constants and above methods, we studied the carbonate system of the Razdol'naya River-Amur Bay estuary in two expeditions of July 2001, the first in a period of average water level and the second after a flood. In the latter survey, extremely low values (∼60 μatm) of pCO2 (carbon dioxide partial pressure) were recorded in the seaward part of the estuary and extremely high (∼13300 μatm) were noted in the river. High pCO2 in the surface water was caused by intense bacterial activity, and low levels were caused by phytoplankton bloom. The nonconservative behavior of the total alkalinity and dissolved inorganic carbon was revealed in the estuary. Based on the data of the carbonate system, the production/destruction of organic matter was assessed.",

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author = "Tishchenko, {P. Ya} and Wong, {C. S.} and Volkova, {T. I.} and Gramm-Osipov, {L. M.} and Johnson, {V. K.} and Dudarev, {O. V.} and Zvalinskii, {V. I.} and Nedashkovskii, {A. P.} and Pavlova, {G. Yu} and Chichkin, {R. V.} and Sagalaev, {S. G.} and Shevtsova, {O. V.} and Shkirnikova, {E. M.}",

note = "Funding Information: ACKNOWLEDGMENTS This work was supported by a grant from the Far East Division of the Russian Academy of Sciences (projects 03-3-A-07-061, 03-1-0-07-002, and 03-1-0-07-005). Copyright: Copyright 2008 Elsevier B.V., All rights reserved.",

year = "2005",

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doi = "10.1007/s11179-005-0042-5",

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AU - Tishchenko, P. Ya

AU - Wong, C. S.

AU - Volkova, T. I.

AU - Gramm-Osipov, L. M.

AU - Johnson, V. K.

AU - Dudarev, O. V.

AU - Zvalinskii, V. I.

AU - Nedashkovskii, A. P.

AU - Pavlova, G. Yu

AU - Chichkin, R. V.

AU - Sagalaev, S. G.

AU - Shevtsova, O. V.

AU - Shkirnikova, E. M.

N1 - Funding Information: ACKNOWLEDGMENTS This work was supported by a grant from the Far East Division of the Russian Academy of Sciences (projects 03-3-A-07-061, 03-1-0-07-002, and 03-1-0-07-005). Copyright: Copyright 2008 Elsevier B.V., All rights reserved.

PY - 2005/1

Y1 - 2005/1

N2 - Two methods, the total alkalinity measurement by Bruevich [4] and pH measurement in a cell without liquid junction [11], were suggested for study of the carbonate system of estuaries. Based on new measurements, the empirical equations were obtained for the first and second seawater concentration constants of carbonic acid for the ranges of salinity 0-40‰ and temperatures 0-30°C. Applying the constants and above methods, we studied the carbonate system of the Razdol'naya River-Amur Bay estuary in two expeditions of July 2001, the first in a period of average water level and the second after a flood. In the latter survey, extremely low values (∼60 μatm) of pCO2 (carbon dioxide partial pressure) were recorded in the seaward part of the estuary and extremely high (∼13300 μatm) were noted in the river. High pCO2 in the surface water was caused by intense bacterial activity, and low levels were caused by phytoplankton bloom. The nonconservative behavior of the total alkalinity and dissolved inorganic carbon was revealed in the estuary. Based on the data of the carbonate system, the production/destruction of organic matter was assessed.

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