Spatial Heterogeneity and Vertical Distribution of Nitrogen Forms in Sediments of Qilu Lake
DOI:
https://doi.org/10.54691/2q44p450Keywords:
Qilu Lake; Sediment; Nitrogen Forms; Vertical Distribution.Abstract
To reveal the spatial heterogeneity and vertical distribution characteristics of nitrogen forms in the sediments of Qilu Lake, overlying water and surface sediment samples were collected from 15 sampling sites in June 2023, and sediment core samples were additionally collected from seven representative sites. The occurrence characteristics, release contributions, and interrelationships of various nitrogen fractions in overlying water, surface sediments, and sediment cores were systematically analyzed. The results showed that inorganic nitrogen dominated the nitrogen pool in the overlying water of Qilu Lake, with relatively low NH4+-N concentrations and comparatively higher NO3--N concentrations. Site Q9 exhibited the most pronounced nitrogen enrichment. DIN was the predominant component of DTN. In surface sediments, TN, PMON, SN, and various forms of EN and PMN all exhibited marked spatial heterogeneity, and the high-value zones of different nitrogen pools did not completely overlap, indicating that various nitrogen fractions possess distinct distribution patterns within the lake basin. The release contributions of nitrogen forms in sediment cores differed significantly among lake zones, with the western zone showing the most pronounced inter-site variability. Vertical profiles of sediment cores revealed that NH4+-N concentrations were relatively high in shallow layers at most sites, whereas site Q9 exhibited a distinct increasing trend with depth. NO3--N concentrations fluctuated considerably among sites. PMN generally decreased from shallow to deep layers. TN remained relatively stable with depth at most sites, with only site Q15 showing notable vertical variation. Correlation analysis indicated that, among the labile nitrogen fractions in surface sediments, NH4+-N in EN exhibited the strongest correlations with overlying water NH4+-N, DIN, and DTN, while other labile nitrogen fractions showed relatively weaker correlations with inorganic nitrogen in overlying water. These findings demonstrate that nitrogen fractions in the sediments of Qilu Lake exhibit significant heterogeneity in both spatial and vertical dimensions, and that there exists a strong coupling relationship between the surface labile nitrogen pool and inorganic nitrogen in the overlying water, which can provide a scientific basis for the identification and management of internal nitrogen pollution in the lake.
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