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评估正电子发射断层扫描作为一种可视化地下微生物过程的方法。

Evaluation of positron emission tomography as a method to visualize subsurface microbial processes.

机构信息

Brookhaven National Laboratory, Upton, NY 11973, USA.

出版信息

J Hazard Mater. 2012 Apr 30;213-214:498-501. doi: 10.1016/j.jhazmat.2012.01.037. Epub 2012 Jan 18.

Abstract

Positron emission tomography (PET) provides spatiotemporal monitoring in a nondestructive manner and has higher sensitivity and resolution relative to other tomographic methods. Therefore, this technology was evaluated for its application to monitor in situ subsurface bacterial activity. To date, however, it has not been used to monitor or image soil microbial processes. In this study, PET imaging was applied as a "proof-of-principle" method to assess the feasibility of visualizing a radiotracer labeled subsurface bacterial strain (Rahnella sp. Y9602), previously isolated from uranium contaminated soils and shown to promote uranium phosphate precipitation. Soil columns packed with acid-purified simulated mineral soils were seeded with 2-deoxy-2-[(18)F]fluoro-D-glucose ((18)FDG) labeled Rahnella sp. Y9602. The applicability of [(18)F]fluoride ion as a tracer for measuring hydraulic conductivity and (18)FDG as a tracer to identify subsurface metabolically active bacteria was successful in our soil column studies. Our findings indicate that positron-emitting isotopes can be utilized for studies aimed at elucidating subsurface microbiology and geochemical processes important in contaminant remediation.

摘要

正电子发射断层扫描(PET)以非破坏性的方式提供时空监测,与其他断层扫描方法相比具有更高的灵敏度和分辨率。因此,该技术已被评估用于原位监测地下细菌活性。然而,迄今为止,它尚未用于监测或成像土壤微生物过程。在这项研究中,PET 成像被用作“原理验证”方法,以评估可视化放射性示踪剂标记的地下细菌菌株(Rahnella sp. Y9602)的可行性,该菌株先前从铀污染土壤中分离出来,被证明能促进磷酸铀沉淀。用酸纯化模拟矿物土壤填充的土壤柱中接种了 2-脱氧-2-[(18)F]氟-D-葡萄糖((18)FDG)标记的 Rahnella sp. Y9602。[(18)F]氟离子作为测量水力传导率的示踪剂和 (18)FDG 作为鉴定地下代谢活跃细菌的示踪剂的适用性在我们的土壤柱研究中是成功的。我们的研究结果表明,正电子发射同位素可用于阐明在污染物修复中重要的地下微生物学和地球化学过程。

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