Unconventional microbial mechanisms for the key factors influencing inorganic nitrogen removal in stormwater bioretention columns

被引:20
|
作者
Huang, Liuqin [1 ,2 ]
Luo, Junyue [1 ]
Li, Linxin [1 ]
Jiang, Hongchen [1 ,2 ]
Sun, Xiaoxi [1 ]
Yang, Jian [1 ]
She, Weiyu [1 ]
Liu, Wen [1 ]
Li, Liqing [3 ]
Davis, Allen P. [4 ]
机构
[1] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
[2] China Univ Geosci, State Environm Protect Key Lab Source Apportionme, Hubei Key Lab Yangtze Catchment Environm Aquat Sc, Wuhan 430074, Peoples R China
[3] China Univ Geosci, Sch Environm Sci, Wuhan 430074, Peoples R China
[4] Univ Maryland, Dept Civil & Environm Engn, College Pk, MD 20742 USA
基金
中国国家自然科学基金;
关键词
Bioretention; Nitrogen pollution; Nitrification; Saturation zone; Denitrification; NITRATE REMOVAL; SP-NOV; AEROBIC DENITRIFICATION; COMPLETE NITRIFICATION; HALOPHILIC ARCHAEON; POLLUTANT REMOVAL; RETENTION; COMMUNITY; BACTERIA; SULFIDE;
D O I
10.1016/j.watres.2021.117895
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Bioretention systems are environmentally friendly measures to control the amount of water and pollutants in urban stormwater runoff, and their treatment performance for inorganic N strongly depends on various microbial processes. However, microbial responses to variations of N mass reduction in bioretention systems are complex and poorly understood, which is not conducive to management designs. In the present study, a series of bioretention columns were established to monitor their fate performance for inorganic N (NH4+ and NO3-) by using different configurations and by dosing with simulated stormwater events. The results showed that NH4+ was efficiently oxidized to NO3-, mainly by ammonia-and nitrite-oxidizing bacteria in the oxic media, regardless of the configurations of the bioretention systems or stormwater conditions. In contrast, NO3- removal pathways varied greatly in different columns. The presence of vegetation efficiently improved NO3- mass reduction through root assimilation and enhancement of microbial NO3- reduction in the rhizosphere. The construction of an organic-rich saturation zone can make the redox potential too low for heterotrophic denitrification to occur, so as to ensure high NO3- mass reduction mainly via stimulating chemolithotrophic NO3- reduction coupled with oxidation of reductive sulfur compounds derived from the bio-reduction of sulfate. In contrast, in the organic-poor saturation zone, multiple oligotrophic NO3- reduction pathways may be responsible for the high NO3- mass reduction. These findings highlight the necessity of considering the variation of N bio-transformation pathways for inorganic N removal in the configuration of bioretention systems.
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页数:13
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