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[中国黄河高浓度铵的成因]

[Reasons of high concentration ammonium in Yellow River, China].

作者信息

Zhang Xue-qing, Xia Xing-hui, Yang Zhi-feng

机构信息

State Key Joint Laboratory of Environmental Simulation and Pollution Control, School of Environment, Beijing Normal University, Beijing 100875, China.

出版信息

Huan Jing Ke Xue. 2007 Jul;28(7):1435-41.

Abstract

Ammonium nitrogen contamination is one of the major problems of the Yellow River in China. The speciation, concentration and sources of nitrogen compounds as well as the water environment conditions of the Yellow River had been analyzed to study the reasons for the fact that the ammonium nitrogen concentration was above the water quality standard. In addition, laboratory experiments had been carried out to investigate the effects of suspended sediment (SS) on nitrification rate. The results indicated that the presence of SS could accelerate the nitrification process, therefore, the effects of SS on nitrification rate was not the reason for the high level of ammonium nitrogen in the river. The excessive and continuous input of nitrogen contaminants to the river was the fundamental reason for the high concentration of ammonium nitrogen. Organic and ammonium nitrogen with high concentration inhibitted the nitrification processes. When the initial NH4+ -N concentrations were 10.1, 18.4 and 28.2 mg/L, nitrification efficiencies were 17.4%, 13.0% and 2.5%, respectively. When the initial organic nitrogen concentrations were 5.5 and 8.6 mg/L, the maximum concentrations of ammonium nitrogen produced by the oxidation of organic nitrogen would reach 0.47 and 1.69 mg/L and they would last for 2 days and 6 days, respectively. The oxygen-consuming organics and toxic substance existing in the river water could inhibit the activity of nitrifying bacteria, and thus lead to the accumulation of ammonium nitrogen. In addition, the high pH value of river water resulted in the high concentration of nonionic ammonium nitrogen which would reduce the activity of nitrifying bacteria and decrease the nitrification rates. Besides, low river runoff, low SS content and low activity of nitrifying bacteria resulted in the high level of ammonium nitrogen of the river in the low water season.

摘要

氨氮污染是中国黄河面临的主要问题之一。为研究黄河氨氮浓度超标原因,对黄河氮化合物的形态、浓度和来源以及水环境状况进行了分析。此外,还开展了实验室实验,以研究悬浮泥沙(SS)对硝化速率的影响。结果表明,SS的存在可加速硝化过程,因此,SS对硝化速率的影响并非黄河氨氮含量高的原因。氮污染物过量且持续输入河流是氨氮浓度高的根本原因。高浓度的有机氮和氨氮抑制了硝化过程。当初始NH4+-N浓度分别为10.1、18.4和28.2mg/L时,硝化效率分别为17.4%、13.0%和2.5%。当初始有机氮浓度分别为5.5和8.6mg/L时,有机氮氧化产生的氨氮最大浓度将分别达到0.47和1.69mg/L,且分别持续2天和6天。河水中存在的耗氧有机物和有毒物质会抑制硝化细菌的活性,从而导致氨氮积累。此外,河水的高pH值导致非离子氨氮浓度升高,这会降低硝化细菌的活性并降低硝化速率。此外,河流径流低、SS含量低和硝化细菌活性低导致河流在枯水期氨氮含量高。

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