4.7 Article

Effects of nitrogen stress on uptake and translocation of organophosphate esters by watermifoil (Myriophyllum aquaticum L.) in an aquatic ecosystem

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SPRINGER HEIDELBERG
DOI: 10.1007/s11356-023-29124-1

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Organophosphate esters; Nitrogen; Plant; K-OW; K-OC; Root uptake

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This study investigates the effects of different nitrogen (N) levels on the uptake and translocation of organophosphate esters (OPEs) by watermifoil (Myriophyllum aquaticum). The results indicate that N levels can alter the uptake, accumulation, and translocation of OPEs in M. aquaticum, with low concentrations of N promoting OPE uptake and high concentrations inhibiting plant growth and OPE accumulation. Additionally, physicochemical parameters, substituents, and structures of OPEs also play a role in their accumulation and translocation in M. aquaticum.
Although organophosphate esters (OPEs) and nitrogen (N) are normally present in aquatic environments, the effects of the plant uptake, accumulation, and translocation of OPEs in different levels of N remain ambiguous. To better understand these processes, watermifoil (Myriophyllum aquaticum L.) as tested plant was chosen to investigate the effects of different N levels on the uptake and translocation of OPEs by plants in matched water-sediment-plant samples. After two months, we found the root-water concentration factors, root-sediment concentration factors, and translocation factors (TFs) were significantly changed with the levels of N (p < 0.05), implying that the presence of N could alter uptake, accumulation, and translocation of OPEs in M. aquaticum, particularly the process of root absorption. Low concentrations of N could remarkably promote the uptake of OPEs by M. aquaticum. However, when the concentrations of N in water were higher than 200 mg/L, the plants' growth and OPE accumulation by M. aquaticum were obviously inhibited with the elevated N contents. Moreover, the enrichment and environmental transport of OPEs in M. aquaticum seemed to be closely associated with physicochemical parameters; the octanol-water partition coefficient had significant relationships with measured organic carbon-normalized sediment-water partition coefficients and TFs in the present study. Additionally, the substituents and structures of OPEs could also affect the accumulation and translocation of OPEs in M. aquaticum, including the chlorination degree and alkyl chain length. This study could improve our understanding of uptake and translocation of OPEs in aquatic plants under different levels of N.

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