Insight into the dynamics of dissolved organic matter components under latitude change perturbation

• Published in: Ecotoxicology and environmental safety Vol. 269; p. 115734
• Main Authors: Jia, Liming, Yang, Qi, Cui, Hongyang
• Format: Journal Article
• Language: English
• Published: Netherlands Elsevier 01.01.2024
• Subjects: 2DCOS; Dissolved organic matter; EEM-PARAFAC; Inner evolutions; Latitude perturbation; EEM-PARAFAC; Inner evolutions; Dissolved organic matter; Latitude perturbation; 2DCOS
• ISSN: 0147-6513; 1090-2414
• DOI: 10.1016/j.ecoenv.2023.115734

Dissolved organic matter (DOM) which can help the transportation of nutrients and pollutants plays essential role in the aquatic ecosystems. However, the dynamics of individual DOM component under the change of latitude have not been elucidated to date. The composition and dynamics of DOM were assessed in this study. Two individual parallel factor analysis (PARAFAC) components were found in each sampling site in Heilongjiang. To further characterize the inner change of the identified PARAFAC components, two-latitude correlation spectroscopy (2DCOS) technique was applied to the excitation loadings data. Interestingly, not all the fluorophore in a PARAFAC component change in the same direction as the overall change of a component. From upstream to downstream, the peak A1 in PARAFAC component C1 showed a downward trend, but peak A2 presented an upward trend. In PARAFAC component C2, the peak T2 and peak T3 showed an inverse changing trend under latitude perturbation. Furthermore, basic nutrients parameters in Heilongjiang were also characterized in each sampling sites. The relationships between DOM and nutrients showed that component C1 made a significant contribution to chemical oxygen demand (COD) and biochemical oxygen demand (BOD5). The evolutions of DOM peak A1 and peak A2 were accompanied by the changing of Total phosphorus (TP). The findings in this study could make a contribution to explore the fate of DOM in high humic-like substance containing river.