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Ammonium concentrations in produced waters from a mesothermic oil field subjected to nitrate injection decrease through formation of denitrifying biomass and anammox activity

机译:经硝酸盐注入的中温油田采出水中的铵浓度通过形成反硝化生物质和厌氧氨氧化活性而降低

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摘要

Community analysis of a mesothermic oil field, subjected to continuous field-wide injection of nitrate to remove sulfide, with denaturing gradient gel electrophoresis (DGGE) of PCR-amplified 16S rRNA genes indicated the presence of heterotrophic and sulfide-oxidizing, nitrate-reducing bacteria (hNRB and soNRB). These reduce nitrate by dissimilatory nitrate reduction to ammonium (e.g., Suifurospirillum and Denitrovibrio) or by denitrification (e.g., Sulfurimonas, Arcobacter, and Thauera). Monitoring of ammonium concentrations in producing wells (PWs) indicated that denitrification was the main pathway for nitrate reduction in the field: breakthrough of nitrate and nitrite in two PWs was not associated with an increase in the ammonium concentration, and no increase in the ammonium concentration was seen in any of 11 producing wells during periods of increased nitrate injection. Instead, ammonium concentrations in produced waters decreased on average from 0.3 to 0.2 mM during 2 years of nitrate injection. Physiological studies with produced waterderived hNRB microcosms indicated increased biomass formation associated with denitrification as a possible cause for decreasing ammonium concentrations. Use of anammox-specific primers and cloning of the resulting PCR product gave clones affiliated with the known anammox genera "Candidatus Brocadia" and "Candidatus Kuenenia," indicating that the anammox reaction may also contribute to declining ammonium concentrations. Overall, the results indicate the following: (i) that nitrate injected into an oil field to oxidize sulfide is primarily reduced by denitrifying bacteria, of which many genera have been identified by DGGE, and (ii) that perhaps counterintuitively, nitrate injection leads to decreasing ammonium concentrations in produced waters.
机译:对一个中温油田进行群落分析,在油田范围内连续注入硝酸盐以去除硫化物,对PCR扩增的16S rRNA基因进行变性梯度凝胶电泳(DGGE),表明存在异养和硫化物氧化硝酸盐还原细菌(hNRB和soNRB)。这些通过异化硝酸盐还原为铵(例如,Suifurospirillum 和 Denitrovibrio)或反硝化作用(例如,硫单胞菌、Arcobacter 和 Thauera)来还原硝酸盐。对生产井(PWs)中铵浓度的监测表明,反硝化作用是该油田减少硝酸盐的主要途径:两个PW中硝酸盐和亚硝酸盐的突破与铵浓度的增加无关,在硝酸盐注入增加期间,11口生产井中的任何一口井的铵浓度都没有增加。相反,在硝酸盐注入的2年中,采出水中的铵浓度平均从0.3mM下降到0.2mM。对采出水源性hNRB微观世界的生理学研究表明,与反硝化作用相关的生物量形成增加是铵浓度降低的可能原因。使用厌氧氨氨酯特异性引物和克隆所得PCR产物,可得到与已知厌氧氨氧化属“Candidatus Brocadia”和“Candidatus Kuenenia”相关的克隆,表明厌氧氨氧化反应也可能导致铵浓度下降。总体而言,结果表明以下几点:(i)注入油田以氧化硫化物的硝酸盐主要通过反硝化细菌来减少,DGGE已经鉴定出许多属,以及(ii)可能与直觉相反,硝酸盐注入导致采出水中铵浓度降低。

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