首页> 外文期刊>Journal of Contaminant Hydrology >Simultaneous influence of indigenous microorganism along with abiotic factors controlling arsenic mobilization in Brahmaputra floodplain, India
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Simultaneous influence of indigenous microorganism along with abiotic factors controlling arsenic mobilization in Brahmaputra floodplain, India

机译:印度雅鲁藏布江洪泛区中土著微生物与非生物因子同时控制砷迁移的同时影响

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In the dynamic cycling of oxic and anoxic aqueous alluvial aquifer environments, varying Arsenic (As) con centrations are controlled by both abiotic and biotic factors. Studies have shown a significant form of toxic As (III) being released through the reductive dissolution of iron-oxy/hydroxide minerals and microbial reduction mechanisms, which leads to a serious health concern. The present study was performed in order to assess the abiotic and biotic factors influencing As release into the alluvial aquifer groundwater in Brahmaputra floodplain, India. The groundwater chemistry, characterization of the sediments, isolation, identification and character ization of prominent As releasing indigenous bacterium were conducted. The measured solid and liquid phases of total As concentration were ranged between 0.02 and 17.2mgkg(-1) and 8 to 353 mu G L-1, respectively. The morphology and mineralogy showed the presence of detrital and authigenic mineral assemblages whereas pri mary and secondary As bearing Realgar and Claudetite minerals were identified, respectively. Furthermore, significant non-labile As fraction was found associated with the amorphous oxides of Fe, Mn and A1. The ob served groundwater chemistry and sediment color, deduced a sub-oxic reducing aquifer conditions in As-con taminated regions. In addition, 16S rDNA sequencing results of the isolated bacterium showed the prominent Pseudomonas aeruginosa responsible for the mobilization of As, reducing condition, biommeralization and causing grey color to the sediments at the shallower and deeper aquifers in the study area. These findings suggest that microbial metabolic activities are equally responsible in iron-oxy/hydroxide reductive dissolution, controlling As mobilization in dynamic fluvial flood plains.
机译:在有氧和无氧冲积含水层环境的动态循环中,不同生物和生物因素都控制着不同浓度的砷(As)。研究表明,通过铁-氧/氢氧化铁矿物质的还原溶解和微生物还原机制释放了一种重要形式的有毒砷(III),这引起了严重的健康问题。进行本研究是为了评估影响印度Brahmaputra洪泛区冲积含水层地下水中As释放的非生物和生物因素。进行了地下水化学,沉积物表征,分离,鉴定和表征了主要的释放As的土著细菌。测得的总砷浓度的固相和液相分别在0.02和17.2mgkg(-1)和8到353μG L-1之间。形态学和矿物学表明碎屑和自生矿物组合的存在,而分别鉴定出主要和次要的含雄黄和克拉德石的矿物。此外,发现与Fe,Mn和Al的无定形氧化物有关的明显的非不稳定As组分。观察到的地下水化学性质和沉积物颜色,推导了被As污染地区的低氧还原含水层条件。此外,分离出的细菌的16S rDNA测序结果显示,铜绿假单胞菌可引起As的动员,减少状况,生物矿化作用,并导致研究区域浅层和深层含水层的沉积物出现灰色。这些发现表明,微生物的代谢活动在氧化铁/氢氧化物的还原溶解中起着同样的作用,从而控制了河流动态洪泛平原中的砷迁移。

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