流入水中の無機窒素が受容盆地の堆積物によって制御される溶存有機物の変換を支配する

Frequent Water Diversion Project significantly regulates the biogeochemical processes and water quality of surface systems, yet it remains poorly understood how recipient basin sediments respond to the inflowing water for mediating the dynamic transformation of dissolved organic matter (DOM). This study systematically conducted a long-term incubation experiment to simulate the interactions of recipient sediments of Dongping Lake, China, with the inflowing waters from different sources. Results showed the significant divergence and heterogenization in aromaticity and molecular weight of DOM in the overlying layer after a 75 day-incubation, during which sunlight irradiation and inorganic nitrogen levels were key in driving the biogeochemical transformation. Metagenomic analyses confirmed that inorganic nitrogen concentrations in the inflowing water governed microbial community succession, with Proteobacteria and Cyanobacteria sensibly responding to nitrogen level fluctuations. Further, nitrate and ammonia nitrogen influenced dissimilatory nitrate reduction activity and exerted positive feedback on the refractory carboxylic-rich alicyclic molecules (CRAM) metabolisms, thereby controlling the aromatization or humification processes of DOM. Specially, compositional characteristics of DOM were primarily determined by the abundance and activity of key functional genes, including narG, narZ, nxrA, narH, narY, nxrB, narI, and narV. This study provides new insights into the significant role of the Water Diversion Project in determining the dissolved organic carbon pool of inflowing water in recipient basins, enhancing biogeochemical understanding of its water quality responses.