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Autotrophic, Hydrogen-Oxidizing, Denitrifying Bacteria in Groundwater, Potential Agents for Bioremediation of Nitrate Contamination

机译:地下水中的自养,氢氧化,反硝化细菌,硝酸盐污染生物修复的潜在剂

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Addition of hydrogen or formate significantly enhanced the rate of consumption of nitrate in slurried core samples obtained from an active zone of denitrification in a nitrate-contaminated sand and gravel aquifer (Cape Cod, Mass.). Hydrogen uptake by the core material was immediate and rapid, with an apparent Km of 0.45 to 0.60 μM and a Vmax of 18.7 nmol cm-3 h-1 at 30°C. Nine strains of hydrogen-oxidizing denitrifying bacteria were subsequently isolated from the aquifer. Eight of the strains grew autotrophically on hydrogen with either oxygen or nitrate as the electron acceptor. One strain grew mixotrophically. All of the isolates were capable of heterotrophic growth, but none were similar to Paracoccus denitrificans, a well-characterized hydrogen-oxidizing denitrifier. The kinetics for hydrogen uptake during denitrification were determined for each isolate with substrate depletion progress curves; the Kms ranged from 0.30 to 3.32 μM, with Vmaxs of 1.85 to 13.29 fmol cell-1 h-1. Because these organisms appear to be common constituents of the in situ population of the aquifer, produce innocuous end products, and could be manipulated to sequentially consume oxygen and then nitrate when both were present, these results suggest that these organisms may have significant potential for in situ bioremediation of nitrate contamination in groundwater.
机译:氢或甲酸盐的添加显着提高了浆状岩心样品中硝酸盐的消耗速率,该岩浆样品是从硝酸盐污染的砂砾石含水层(马萨诸塞州科德角)的反硝化活性区获得的。核心材料立即吸收氢气,在30°C下的表观Km为0.45至0.60μM,Vmax为18.7 nmol cm-3 h-1。随后从含水层中分离出九种氢氧化反硝化细菌菌株。其中八株在氧或硝酸盐为电子受体的氢上自养生长。一种菌株混合营养生长。所有的分离物都能够异养生长,但是没有一个与特征充分的氢氧化反硝化剂反硝化副球菌相似。用底物消耗进度曲线确定每个分离物在反硝化过程中氢吸收的动力学。 Kms范围为0.30至3.32μM,Vmax为1.85至13.29 fmol cell-1 h-1。由于这些生物似乎是含水层原位种群的共同组成部分,会产生无害的最终产品,并且可以被操纵以依次消耗氧气和硝酸盐(如果两者都存在),因此这些结果表明这些生物可能具有巨大的潜力。地下水中硝酸盐污染的原位生物修复。

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