Constituents of organic alkalinity in pore water of marine sediments

In this study we investigated the components of organic alkalinity (A(O)) in pore water from marine sediments. We used absorbance and fluorescence of pore water to characterize dissolved organic matter (DOM), the source of A(O). Research material was collected during growing season (September 2016) from two sites located in the eutrophic Gulf of Gdansk (southern Baltic). Concentration of Ao ranged from 104 to 1505 mu mol(-1) and increased with sediment depth. Our results demonstrate a clear link between Ao and composition of DOM in pore water. Measurements of pore water fluorescence showed that the main source of A(o) is humic substances. The protein-like fluorescence, pointing to presence of freshly produced organic substances, was clearly visible in the upper layers and diminished with depth. There are changes in absorbance spectra with depth indicating decrease of molecular weight of DOM. In anoxic sediments the concentration of A(o) was close to the alkalinity from non-carbonate inorganic bases (N-CIBs) and did not exceed 8% of total alkalinity (A(T)). In the sediments where organic matter was mineralized with the use of substances preceding sulfate in the sequence of oxidants (i.e. oxygen, nitrate, Mn, Fe), DOM was the source of up to 17% of A(T). The results from this study indicate that DOM has a large effect on acid neutralizing capacity of pore water of marine sediments. We suggest the production of A(o) in sediment and its benthic efflux should be taken into account in modeling acid-base system in shelf seas.