Abstract
The processes regulating the concentration and isotopic composition of dissolved inorganic carbon (DIC) in pore water were investigated in three different parts of Lake Bled. It was found that the isotopic composition of dissolved inorganic carbon (DIC) is strongly influenced by methanogenesis. Simple diagenetic model reproduces the observed carbonisotope profiles and the DIC concentration data resonably well in investigated parts. This findings lead us to conclude that the majority of processes affecting DIC are taken into account in the model.
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