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弥河沉积物的反硝化和厌氧氨氧化过程

本站小编 Free考研考试/2022-02-11

弥河沉积物的反硝化和厌氧氨氧化过程
其他题名Denitrification and anammox processes in sediment of Mihe River, China
李佳霖1,2; 秦松1,2
发表期刊中国环境科学
ISSN1000-6923
2021
卷号41期号:4页码:1588-1596
关键词反硝化作用厌氧氨氧化作用功能微生物影响因素弥河
研究领域Environmental Sciences & Ecology
英文摘要Four sites were selected along Mihe River to sample the sediments and characterize physiochemical property to reveal denitrification/anammox processes and their constraints by isotope tracing experiment and molecular biological analysis. The results showed that the rates of denitrification varied from 151.75 to 2847.86mumol/(m2 ·h), and the anammox rates were in the range of 149.57 to 2109.17mumol/(m2 ·h). The relative contribution of anammox in the nitrogen removal was in an average of 56.1%. The nirK type was the dominant denitrifier with the abundance of 0.19*10~6~5.12*10~6 copies/g in the sediment, which was in the phylum of alpha- and beta- Proteobacteria. The anammox bacteria marked by hzsA gene was in the range of 2.58*10~2~1.14*10~4 copies/g, which belonged to the Ca. Brocadia clades in Planctomycetes. Furthermore, the denitrification rate was positively related with TN content and PO4 3- concentration, while the anammox rate was positively related with TN content and negatively related with sediment density. The physiochemical property of sediment was the main condition determining the nitrogen removal rates. The results highlight that denitrification and anammox were of great significance to reduce nitrogen eutrophication, and sediment environment treatment was a considerable way to regular nitrogen removal rate.
中文摘要本研究选取弥河4个站点为研究对象,在不同季节分别采集沉积物样品,测定理化指标,并采用同位素配对技术和分子生物学方法,研究了沉积物中的反硝化和厌氧氨氧化作用及其影响因素.结果表明,弥河沉积物中的反硝化速率变化范围为151.75~2847.86mumol/(m2 ·h),厌氧氨氧化速率的变化范围为149.57~2109.17mumol/(m2 ·h),厌氧氨氧化在氮去除中的贡献量平均达到56.1%.沉积物中的反硝化细菌以nirK型为主,丰度为0.19*10~6~5.12*10~6个/g,主要是alpha-和beta-变形菌门;厌氧氨氧化细菌以hzsA为标记基因的丰度范围是2.58*10~2~1.14*10~4个/g,主要为浮霉菌门的Brocadia属细菌.反硝化速率与沉积物中的TN含量和间隙水PO4 3-呈正相关关系,厌氧氨氧化作用与沉积物中的TN含量呈正相关,而与沉积物密度呈负相关关系,沉积物的理化指标是决定氮去除速率的主要环境条件.弥河的反硝化和厌氧氨氧化作用明显,对减轻氮超标具有重要意义,合理改变沉积环境是有效提高氮去除速率的可参考方式.
文章类型Article
资助机构国家自然科学基金资助项目
收录类别CSCD
语种中文
CSCD记录号CSCD:6950557
引用统计
文献类型期刊论文
条目标识符http://ir.yic.ac.cnhttp://ir.yic.ac.cn/handle/133337/30289
专题海岸带生物学与生物资源利用重点实验室_海岸带生物学与生物资源保护实验室

作者单位1.中国科学院烟台海岸带研究所海岸带生物学与生物资源保护实验室,山东烟台264003;
2.中国科学院海洋大科学研究中心,山东青岛266071

推荐引用方式
GB/T 7714李佳霖,秦松. 弥河沉积物的反硝化和厌氧氨氧化过程[J]. 中国环境科学,2021,41(4):1588-1596.
APA李佳霖,&秦松.(2021).弥河沉积物的反硝化和厌氧氨氧化过程.中国环境科学,41(4),1588-1596.
MLA李佳霖,et al."弥河沉积物的反硝化和厌氧氨氧化过程".中国环境科学 41.4(2021):1588-1596.


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