地下水
环境化学
稳定同位素探测
细菌
乙酸钠
不动杆菌
化学
环境科学
含水层
沉积物
生物
微生物
微生物种群生物学
铀
乙酸乙酯
生物修复
微生物学
稳定同位素比值
微生物生态学
生态学
领域(数学)
大肠杆菌
分数(化学)
同位素
肠杆菌科
相(物质)
作者
Lee J. Kerkhof,Kenneth H. Williams,Philip E. Long,Lora R. McGuinness
摘要
Previous experiments at the Rifle, Colorado Integrated Field Research Challenge (IFRC) site demonstrated that field-scale addition of acetate to groundwater reduced the ambient soluble uranium concentration. In this report, sediment samples collected before and after acetate field addition were used to assess the active microbes via (13)C acetate stable isotope probing on 3 phases [coarse sand, fines (8-approximately 150 μm), groundwater (0.2-8 μm)] over a 24-day time frame. TRFLP results generally indicated a stronger signal in (13)C-DNA in the "fines" fraction compared to the sand and groundwater. Before the field-scale acetate addition, a Geobacter-like group primarily synthesized (13)C-DNA in the groundwater phase, an alpha Proteobacterium primarily grew on the fines/sands, and an Acinetobacter sp. and Decholoromonas-like OTU utilized much of the (13)C acetate in both groundwater and particle-associated phases. At the termination of the field-scale acetate addition, the Geobacter-like species was active on the solid phases rather than the groundwater, while the other bacterial groups had very reduced newly synthesized DNA signal. These findings will help to delineate the acetate utilization patterns of bacteria in the field and can lead to improved methods for stimulating distinct microbial populations in situ.
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