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The Marine Carbonate System: Ionic Interactions and Biogeochemical Processes


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Title: The Marine Carbonate System: Ionic Interactions and Biogeochemical Processes
Authors: Ulfsbo, Adam
E-mail: ulfsbo@chem.gu.se
Issue Date: 7-May-2014
University: University of Gothenburg. Faculty of Science
Institution: Department of Chemistry and Molecular Biology ; Institutionen för kemi och molekylärbiologi
Parts of work: I. Ulfsbo, A., Hulth, S., Anderson, L. G. (2011), pH and biogeochemical processes in the Gotland Basin of the Baltic Sea, Marine Chemistry, 127, 20-30.
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II. Abbas, Z., Ulfsbo, A., Turner, D. R. (2013). Monte Carlo simulation of the dissociation constants of CO2 in 0 to 1 molal sodium chloride between 0 and 25 C, Marine Chemistry, 150, 1-10.
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III. Ulfsbo, A., Cassar, N., Korhonen, M., van Heuven, S., Hoppema, M., Kattner, G., Anderson, L. G. (2014). Late summer net community production in the central Arctic Ocean using multiple approaches, Global Biogeochemical Cycles, submitted February 2014.

IV. Ericson, Y., Ulfsbo, A., van Heuven, S., Kattner, G., Anderson, L. G. (2014). Increasing carbon inventory of the intermediate layers of the Arctic Ocean, Journal of Geophysical Research: Oceans.
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V. Ulfsbo, A., Kulinski, K., Anderson, L. G., Turner, D.R. (2014). Modelling organic alkalinity in the Baltic Sea using a Humic-Pitzer approach, manuscript in preparation for Marine Chemistry.

VI. Ulfsbo, A., Abbas, Z., Turner, D. R. (2014). Activity coefficients of a simplified seawater electrolyte at varying salinity (5-40) and temperature (0-25 C) using Monte Carlo simulations, manuscript in preparation for Marine Chemistry.
Date of Defence: 2014-05-28
Disputation: Onsdagen den 28 maj 2014, kl. 10.00, Sal KB, Kemigården 4
Degree: Doctor of Philosophy
Publication type: Doctoral thesis
Keywords: Marine
seawater
carbonate system
CO2
Arctic Ocean
Baltic Sea
organic alkalinity
Pitzer
Monte Carlo
activity coefficients
biogeochemical processes
Abstract: The absorption of atmospheric carbon dioxide (CO2) by seawater and subsequent equilibrium reactions within this ionic medium give rise to a complex chemical system often referred to as the marine carbonate system. This system is influenced by physical and biogeochemical processes in the ocean. The marine carbonate system is a major component of the global carbon cycle and is, by virtue of its interaction with atmospheric CO2, of fundamental importance to the Earth’s climate. Accurate knowl... more
ISBN: 978-91-628-8998-2
URI: http://hdl.handle.net/2077/35246
Appears in Collections:Doctoral Theses from University of Gothenburg / Doktorsavhandlingar från Göteborgs universitet
Doctoral Theses / Doktorsavhandlingar Institutionen för kemi och molekylärbiologi

 

 

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