Department of Biology, University of Waterloo, Waterloo, Ontario, N2L 3G1, Canada.
Department of Chemistry, Western University, London, Ontario, N6A 3K7, Canada.
J Appl Microbiol. 2024 Mar 1;135(3). doi: 10.1093/jambio/lxae053.
Many countries are in the process of designing a deep geological repository (DGR) for long-term storage of used nuclear fuel. For several designs, used fuel containers will be placed belowground, with emplacement tunnels being backfilled using a combination of highly compacted powdered bentonite clay buffer boxes surrounded by a granulated "gapfill" bentonite. To limit the potential for microbiologically influenced corrosion of used fuel containers, identifying conditions that suppress microbial growth is critical for sustainable DGR design. This study investigated microbial communities in powdered and gapfill bentonite clay incubated in oxic pressure vessels at dry densities between 1.1 g cm-3 (i.e. below repository target) and 1.6 g cm-3 (i.e. at or above repository target) as a 1-year time series.
Our results showed an initial (i.e. 1 month) increase in the abundance of culturable heterotrophs associated with all dry densities <1.6 g cm-3, which reveals growth during transient low-pressure conditions associated with the bentonite saturation process. Following saturation, culturable heterotroph abundances decreased to those of starting material by the 6-month time point for all 1.4 and 1.6 g cm-3 pressure vessels, and the most probable numbers of culturable sulfate-reducing bacteria (SRB) remained constant for all vessels and time points. The 16S rRNA gene sequencing results showed a change in microbial community composition from the starting material to the 1-month time point, after which time most samples were dominated by sequences associated with Pseudomonas, Bacillus, Cupriavidus, and Streptomyces. Similar taxa were identified as dominant members of the culture-based community composition, demonstrating that the dominant members of the clay microbial communities are viable. Members of the spore-forming Desulfosporosinus genus were the dominant SRB for both clay and culture profiles.
After initial microbial growth while bentonite was below target pressure in the early phases of saturation, microbial growth in pressure vessels with dry densities of at least 1.4 g cm-3 was eventually suppressed as bentonite neared saturation.
许多国家正在设计用于长期储存乏核燃料的深地质处置库(DGR)。对于一些设计方案,用过的燃料容器将被放置在地下,安置隧道将用充满高度压实的粉末状膨润土缓冲盒和周围的粒状“间隙填充”膨润土混合物回填。为了限制乏核燃料容器受微生物影响腐蚀的可能性,确定抑制微生物生长的条件对于可持续的 DGR 设计至关重要。本研究调查了在充氧压力容器中培养的粉末状和间隙填充膨润土粘土中的微生物群落,这些膨润土粘土的干密度在 1.1 g cm-3(即低于储存库目标)和 1.6 g cm-3(即达到或超过储存库目标)之间,作为一个为期 1 年的时间序列。
我们的研究结果表明,在所有干密度<1.6 g cm-3的情况下,与所有干密度<1.6 g cm-3相关的可培养异养生物的丰度最初(即 1 个月)增加,这表明在膨润土饱和过程中与瞬态低压条件相关的生长。饱和后,所有 1.4 和 1.6 g cm-3压力容器的可培养异养生物丰度在 6 个月时间点下降到起始材料水平,可培养硫酸盐还原菌(SRB)的最可能数量在所有容器和时间点保持不变。16S rRNA 基因测序结果显示,从起始材料到 1 个月时间点,微生物群落组成发生了变化,此后大多数样本主要由与假单胞菌、芽孢杆菌、铜绿假单胞菌和链霉菌相关的序列组成。基于培养的群落组成中也鉴定出了相似的优势类群,这表明粘土微生物群落的优势成员是有活力的。在粘土和培养物的 profiles 中,形成孢子的脱硫孤菌属的成员是 SRB 的主要成员。
在膨润土在早期饱和阶段低于目标压力时,微生物最初生长,然后在膨润土接近饱和时,至少 1.4 g cm-3 干密度的压力容器中的微生物生长最终受到抑制。