Changes of DOM and its correlation with internal nutrient release during cyanobacterial growth and decline in Lake Chaohu, China.

The seasonal changes in dissolved organic matter (DOM), and its correlation with the release of internal nutrients during the annual cycle of cyanobacteria in the eutrophic Lake Chaohu, China, were investigated from four sampling periods between November 2020 and July 2021. The DOM fluorescence components were identified as protein-like C1, microbial humic-like C2, and terrestrial humic-like C3. The highest total fluorescence intensity (F) of DOM in sediments during the incubation stage is due to the decomposition and degradation of cyanobacteria remains.