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芬兰东部一座前试点规模铀矿中的微生物群落——与镭固定有关。

Microbial communities in a former pilot-scale uranium mine in Eastern Finland - Association with radium immobilization.

机构信息

Department of Chemistry, Radiochemistry, Faculty of Science, University of Helsinki, Finland.

Department of Chemistry, Radiochemistry, Faculty of Science, University of Helsinki, Finland.

出版信息

Sci Total Environ. 2019 Oct 10;686:619-640. doi: 10.1016/j.scitotenv.2019.05.432. Epub 2019 Jun 4.

Abstract

The bacterial, fungal and archaeal communities were characterized in 17 top soil organic and mineral layer samples and in top sediment samples of the Paukkajanvaara area, a former pilot-scale uranium mine, located in Eno, Eastern Finland, using amplicon sequencing and qPCR. Soil and sediment samples were in addition analyzed for radium (Ra), sulfate (SO), nitrate (NO) and phosphate (PO) concentrations. New bacterial strains, representing Pseudomonas spp., were isolated from the mine and reference area and used in laboratory experiments on uptake and leaching of radium (Ra). The effect of these strains on the sulfate leaching from the soil samples was also tested in vitro. Between 6 × 10 and 5 × 10 copies g DW (dry weight) of bacterial 16S rRNA genes, 5 × 10-1 × 10 copies g DW archaeal 16S rRNA genes and 1 × 10-1 × 10 copies g DW fungal 5.8S rRNA genes were detected in the samples. A total of 814, 54 and 167 bacterial, archaeal and fungal genera, respectively, were identified. Proteobacteria, Euryarchaeota and Mortiriella were the dominant bacterial, archaeal and fungal phyla, respectively. All tested Pseudomonas spp. strains isolates from Paukkajanvaara removed Ra from the solution, but the amount of removed Ra depended on incubation conditions (temperature, time and nutrient broth). The highest removal of Ra (5320 L/kg DW) was observed by the Pseudomonas sp. strain T5-6-I at 37 °C. All Pseudomonas spp. strains decreased the release of Ra from soil with an average of 23% while simultaneously increasing the concentration of SO in the solution by 11%. As Pseudomonas spp. were frequent in both the sequence data and the cultures, these bacteria may play an important role in the immobilization of Ra in the Paukkajanvaara mine area.

摘要

在芬兰东部 Eno 的 Paukkajanvaara 地区,对一个前试点规模铀矿的 17 个表土有机和矿物质层样本和顶部沉积物样本进行了细菌、真菌和古菌群落特征研究,采用扩增子测序和 qPCR 方法。此外,还分析了土壤和沉积物样本中的镭(Ra)、硫酸盐(SO)、硝酸盐(NO)和磷酸盐(PO)浓度。从该矿和参考区分离出新的细菌菌株,代表假单胞菌属,用于实验室研究镭(Ra)的吸收和浸出。还在体外测试了这些菌株对土壤样本硫酸盐浸出的影响。在样本中检测到 6×10 到 5×10 拷贝 g DW(干重)的细菌 16S rRNA 基因、5×10-1×10 拷贝 g DW 的古菌 16S rRNA 基因和 1×10-1×10 拷贝 g DW 的真菌 5.8S rRNA 基因。共鉴定出 814、54 和 167 个细菌、古菌和真菌属。变形菌门、广古菌门和Mortiriella 分别是主要的细菌、古菌和真菌门。从 Paukkajanvaara 分离出的所有测试的假单胞菌属菌株都从溶液中去除了 Ra,但去除的 Ra 量取决于孵育条件(温度、时间和营养肉汤)。在 37°C 下,假单胞菌属 T5-6-I 菌株观察到最高的 Ra 去除量(5320 L/kg DW)。所有假单胞菌属菌株平均减少了 23%的 Ra 从土壤中的释放,同时将溶液中 SO 的浓度提高了 11%。由于假单胞菌属在序列数据和培养物中都很常见,因此这些细菌可能在 Paukkajanvaara 矿区 Ra 的固定化中发挥重要作用。

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