Yang Li-Biao, Lei Kun, Meng Wei
Huan Jing Ke Xue. 2015 Mar;36(3):905-13.
Ratios of nitrogen loss and N2O production by denitrification were observed in Daliao River and the estuary in summer 2013. The results showed that the concentrations of N and P in the main stream of Daliao River were significant higher than those in the estuary (P < 0.05). Decrease of nutrients concentration in the estuary might be integrally caused by water diluting and biogeochemical processes. The net increase of dissolved N2 (ΔN2) ranged between -11.01 and 71.37 μmol x L(-1), in which the negative values were mostly determined in the main stream of the river, indicating the consumption amount of N2 was higher than the production in the fresh water. The mean ratio of N2O production during the process of denitrification was about 0.007%, and the N2O flux across water-air interface was about 0.04% of the total fluxes (N2O + N2). In this study, ΔN2 was not related with DO, while exhibited a significant positive correlation with water temperature and salinity, and a negative correlation with NO3-. This suggests that denitrification was not totally regulated by DO level in the estuary, and coupled nitrification-denitrification was the main denitrification process. Finally, we estimated that 26% of the TN, 37% of the DIN, and 43% of the NO3- were removed by denitrification in the Daliao River estuary based on the ratio of ΔN2 to N concentrations.
2013年夏季,对辽河及其河口反硝化作用导致的氮损失与N2O产生的比率进行了观测。结果表明,辽河干流中氮和磷的浓度显著高于河口(P < 0.05)。河口营养物质浓度的降低可能是由水体稀释和生物地球化学过程共同造成的。溶解态N2的净增量(ΔN2)在-11.01至71.37 μmol·L-1之间,其中负值大多出现在河流干流中,这表明淡水中N2的消耗量高于产生量。反硝化过程中N2O产生的平均比率约为0.007%,水-气界面的N2O通量约占总通量(N2O + N2)的0.04%。在本研究中,ΔN2与溶解氧(DO)无关,而与水温、盐度呈显著正相关,与硝酸根(NO3-)呈负相关。这表明河口反硝化作用并非完全受DO水平调控,耦合硝化-反硝化是主要的反硝化过程。最后,基于ΔN2与氮浓度的比率,我们估算出辽河河口反硝化作用去除了2(TN)的26%、溶解无机氮(DIN)的37%以及NO3-的43%。