The goal of this work is to study the origin and interrelationships of the different processes affecting the carbonate system transformation during the bloom. Paticularly the biogenic carbonates formation was described and the numerical estimates of this process intensity during the phytoplankton intensive production period were obtained.

The carbon chemical-biological cycle, air-water exchange and carbonate system transformation were described in the model. A special iteration scheme was used to describe the carbonate system balancing after the carbon dioxide consummation took place.

Fig.1. Model scheme of the matter transformation, where:

phyto - phytoplankton, zoo - zooplankton, PO₄-phosphates, POP - particulate organic phosphorus, DOP - dissolved organic phosphorus, TCO₂ - dissolved inorganic carbon, POC - particulate organic carbon, DOC - dissolved organic carbon. Thick arrows correspond to Michaelis-Menten formulation.

Fig.2. Variability of the model components during the phytoplanktom bloom:

Biological parameters and phosphorus compounds.

Fig.3. Variability of the model carbon dioxide components:

Numerical experiment without CaCO₃ precipitation by algaes.

Fig.4. Variability of the model carbon dioxide components:

Numerical experiment with assuming CaCO₃ precipitation by algaes.

On the base of modeling it was shown that the amount of potentially precipitated during the bloom period CaCO₃ should be up to 20 mM l^-1. The changes of carbon alkalinity can reach 0.030 mg-eq l^-1. The differences of carbonate system parameters behavior including CaCO₃ formation is significant enough to be measured during the field investigations of the standard carbonate system parameters with the modern technique accuracy.

The detailed description of this model is in:

Yakushev, E.V., 1996, Modeling of the carbonate system balance changes connected with phytoplankton bloom. Marine Chemistry. (Submitted to Publication).

The text is available here. Thank you for your interest.

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