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土壤缓冲容量可用于优化嗜冷烃类生物修复的生物刺激作用。

Soil Buffering Capacity Can Be Used To Optimize Biostimulation of Psychrotrophic Hydrocarbon Remediation.

机构信息

College of Agriculture and Bioresources, Department of Soil Science, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5A8, Canada.

Department of Physics, University of Regina, Regina, Saskatchewan S4S 0A2, Canada.

出版信息

Environ Sci Technol. 2021 Jul 20;55(14):9864-9875. doi: 10.1021/acs.est.1c01113. Epub 2021 Jun 25.

DOI:10.1021/acs.est.1c01113
PMID:34170682
Abstract

Effective bioremediation of hydrocarbons requires innovative approaches to minimize phosphate precipitation in soils of different buffering capacities. Understanding the mechanisms underlying sustained stimulation of bacterial activity remains a key challenge for optimizing bioremediation-particularly in northern regions. Positron emission tomography (PET) can trace microbial activity within the naturally occurring soil structure of intact soils. Here, we use PET to test two hypotheses: (1) optimizing phosphate bioavailability in soil will outperform a generic biostimulatory solution in promoting hydrocarbon remediation and (2) oligotrophic biostimulation will be more effective than eutrophic approaches. In so doing, we highlight the key bacterial taxa that underlie aerobic and anaerobic hydrocarbon degradation in subarctic soils. In particular, we showed that (i) optimized phosphate bioavailability outperformed generic biostimulatory solutions in promoting hydrocarbon degradation, (ii) oligotrophic biostimulation is more effective than eutrophic approaches, and (iii) optimized biostimulatory solutions stimulated specific soil regions and bacterial consortia. The knowledge gleaned from this study will be crucial in developing field-scale biodegradation treatments for sustained stimulation of bacterial activity in northern regions.

摘要

有效的烃类生物修复需要创新的方法来最大限度地减少不同缓冲能力土壤中的磷酸盐沉淀。了解持续刺激细菌活性的机制仍然是优化生物修复的关键挑战,特别是在北方地区。正电子发射断层扫描 (PET) 可以追踪完整土壤中自然存在的土壤结构内的微生物活性。在这里,我们使用 PET 来检验两个假设:(1)优化土壤中的磷酸盐生物利用度将优于通用生物刺激解决方案,从而促进烃类修复;(2)贫营养生物刺激将比富营养方法更有效。通过这样做,我们突出了在亚北极土壤中支持好氧和厌氧烃类降解的关键细菌类群。特别是,我们表明:(i)优化的磷酸盐生物利用度在促进烃类降解方面优于通用生物刺激解决方案;(ii)贫营养生物刺激比富营养方法更有效;(iii)优化的生物刺激解决方案刺激了特定的土壤区域和细菌联合体。从这项研究中获得的知识对于开发现场规模的生物降解处理方法以持续刺激北方地区的细菌活性至关重要。

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