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Mixing and sulphate-reducing activity of bacteria in swelling, compacted bentonite clay under high-level radioactive waste repository conditions

机译:在高放废物处置库条件下膨胀的致密膨润土中细菌的混合和硫酸盐还原活性

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Aim: The fate of micro-organisms in the bentonite clay surrounding high-level radioactive waste (HLW)-containing copper canisters in a future Swedish underground (500m) repository were investigated. Methods and Results: Laboratory experiments were designed in which the mixing of various bacterial species with swelling bentonite was studied. A clear trend of fewer cultivable bacteria at depth was seen in the clay. This trend was consistent as the incubation time was increased from 8h to 28 weeks. Sulphate-reducing bacteria were found to be active, reducing sulphate at the lowest density studied, 1.5g cm~(3), but sulphate reduction activity ceased at higher densities. Conclusions: The number of viable micro-organisms in an HLW repository bentonite clay buffer will decrease rapidly during swelling and very few viable cells will be present at full compaction. Significance and Impact of the Study: Sulphate-reducing bacteria will most probably not be able to induce corrosion of HLW-containing copper canisters.
机译:目的:研究了未来瑞典地下(500m)处置库中含高放射性废物(HLW)的铜罐周围膨润土中微生物的命运。方法和结果:设计了实验室实验,研究了各种细菌与膨润土的混合。在粘土中可以看到明显的趋势,即在深处可培养细菌减少。随着孵育时间从8小时增加到28周,这种趋势是一致的。发现硫酸盐还原菌具有活性,在研究的最低密度1.5g cm〜(3)时还原硫酸盐,但在较高密度时硫酸盐还原活性停止。结论:在溶胀过程中,HLW膨润土粘土缓冲液中的存活微生物数量将迅速减少,并且在完全压实的情况下,几乎没有存活细胞。研究的意义和影响:减少硫酸盐的细菌极有可能无法诱导含HLW的铜罐的腐蚀。

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