Potential of a novel facultative anaerobic denitrifying Cupriavidus sp. W12 to remove fluoride and calcium through calcium bioprecipitation

被引:60
作者
Liu, Jiaran [1 ,2 ]
Su, Junfeng [1 ,2 ]
Ali, Amjad [1 ,2 ]
Wang, Zhao [1 ,2 ]
Zhang, Ruijie [1 ,2 ]
机构
[1] Xian Univ Architecture & Technol, Sch Environm & Municipal Engn, Xian 710055, Peoples R China
[2] Xian Univ Architecture & Technol, Shaanxi Key Lab Environm Engn, Xian 710055, Peoples R China
基金
中国国家自然科学基金;
关键词
Anaerobic MICP; Denitrification; F-removal; Groundwater; EXTRACELLULAR POLYMERIC SUBSTANCES; PRECIPITATION; WATER; PHOSPHATE; BACTERIA; NITRATE; BIOMINERALIZATION; HYDROXYAPATITE; IDENTIFICATION; NANOPARTICLES;
D O I
10.1016/j.jhazmat.2021.126976
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study focused on a novel denitrifying Cupriavidus sp. W12, which can perform microbial induced calcium precipitation (MICP) to remove fluoride (F-) under aerobic and anaerobic conditions. Under anaerobic condition, the removal ratios of F-, calcium (Ca2+), and nitrate (NO3--N) reached 87.52%, 65.03%, and 96.06%, respectively, which were higher than that under aerobic condition (50.17%, 88.21%, and 67.33%, respectively). Higher pH of 8.26 was obtained after 120 h of the strain W12 growth under anaerobic condition than that under aerobic condition (7.77). The F-removal ratio of 98.20% was predicted by the response surface methodology (RSM). Scanning electron microscopy (SEM) images of anaerobic precipitation were dense and porous. CaCO3, Ca-5(PO4)(3)OH, Ca-5(PO4)(3)F, and CaF2 were determined by X-ray diffraction (XRD) and energy dispersive spectrometer (EDS). Self-aggregation of bacteria and adsorption of biological crystal seeds were the determinant of the precipitates formation. The results of infrared spectrometer (FTIR) and excitation-emission matrix (EEM) showed that anaerobic extracellular polymeric substances (EPS) expression led the proportion of hydroxylapatite in the precipitates increased. As the first report on the anaerobic MICP to remove F-, it provides a theoretical basis for the remediation of F-, Ca2+, and NO3--N in groundwater.
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页数:11
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