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Continuous long-term observations of the carbonate system dynamics in the water column of a temperate fjord

Atamanchuk, Dariia, 1987 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi och molekylärbiologi,Department of Chemistry and Molecular Biology,University of Gothenburg
Kononets, Mikhail Y, 1978 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi och molekylärbiologi,Department of Chemistry and Molecular Biology,University of Gothenburg
Thomas, P. J. (författare)
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Hovdenes, J. (författare)
Tengberg, Anders, 1962 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi och molekylärbiologi,Department of Chemistry and Molecular Biology,University of Gothenburg
Hall, Per, 1954 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi och molekylärbiologi,Department of Chemistry and Molecular Biology,University of Gothenburg
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 (creator_code:org_t)
Elsevier BV, 2015
2015
Engelska.
Ingår i: Journal of Marine Systems. - : Elsevier BV. - 0924-7963. ; 148, s. 272-284
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • A cabled underwater observatory with more than 30 sensors delivering data in real-time was used to study the dynamics of the upper pelagic carbonate system of the Koljo Fjord, western Sweden, from September to April during two consecutive years (2011-2012 and 2012-2013). In the dynamic upper ca 15 m of the water column, salinity and temperature varied by up to 10 and 20 degrees C throughout the recorded periods, respectively. Partial pressure of CO2 (pCO(2)), measured with newly developed optical sensors (optodes) at three water depths (5, 9.6 and 12.6 m), varied between 210-940 mu atm, while O-2 varied between 80-470 mu mol/L. Redfield scaled graphs (Delta O-2:Delta DIC = -1.30), in which DIC was derived from pH or pCO(2) and salinity-derived alkalinity (A(Tsal)), and oxygen was measured by the sensors, were used as a tool to assess timing and occurrence of different processes influencing the dynamics of these parameters. Distinctive short-term variations of pCO(2) and O-2 were induced by either tidal oscillations, wind-driven water mass transport in the mixed layer or occasional transport of deep-basin water from below the thermo/halodine to the surface layer. Intensified air-sea gas exchange during short storm events was usually followed by stabilization of gas-related parameters in the water column, such as O-2 concentration and pCO(2), on longer time-scales characteristic for each parameter. Biological processes including organic matter degradation in late summer/autumn and primary production in early spring were responsible for slower and gradual seasonal changes of pCO(2) and O-2. Net primary production (NPP) rates in the Koljo Fjord were quantified to be 1.79 and 2.10 g C m(-2) during the spring bloom periods in 2012 and 2013, respectively, and ratios of 02 production:DIC consumption during the same periods were estimated to be -1.21 +/- 0.02 (at 5 m depth in 2013), -1.51 +/- 0.02 (at 12.6 m in 2012) and -1.95 +/- 0.05 (at 9.6 m in 2013). These ratios are discussed and compared to previously reported 02:C ratios during primary production. (C) 2015 Elsevier B.V. All rights reserved.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Oceanografi, hydrologi och vattenresurser (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Oceanography, Hydrology and Water Resources (hsv//eng)

Nyckelord

Carbonate system of seawater
Long-term in situ measurements
pCO(2)
Redfield ratio
NPP rates
TOTAL INORGANIC CARBON
LIFETIME-BASED OPTODE
CORE WAVE-GUIDE
BALTIC
SEA
DISSOCIATION-CONSTANTS
PARTIAL-PRESSURE
PROFILING FLOAT
ORGANIC-MATTER
TIME-SERIES
NORTH-SEA
Geosciences
Multidisciplinary
Marine & Freshwater Biology
Oceanography
IGEBRANDT A
1991
LIMNOLOGY AND OCEANOGRAPHY
V36
P444
GRANDPRE MD
1995
LIMNOLOGY AND OCEANOGRAPHY
V40
P969
Marine & Freshwater Biology

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