KU-KIST Green School, Korea University, Seoul, 02841, South Korea.
Korea Atomic Energy Research Institute, Daejeon, 34057, South Korea.
J Environ Manage. 2021 May 1;285:112087. doi: 10.1016/j.jenvman.2021.112087. Epub 2021 Feb 12.
The construction of an underground facility can dramatically change the quality, flow direction, and level of groundwater. It may also impact subsurface microbial composition and activity. Groundwater quality was monitored over eight years in two observational wells near an underground disposal facility on the east coast of South Korea. The results showed dramatic increases in dissolved ions such as O, Na, Ca, Mg, and SO during facility construction. Seepage water samples downgradient from the silos and tunnels, and precipitates deposited along the seepage water flow path were collected to determine the impact inside the disposal facility. X-ray analysis (powder X-ray diffraction (pXRD) and X-ray absorption fine structure (XAFS)) were used to characterize the mineral precipitates. Microbial community composition was determined by 16S rRNA gene sequencing. The seepage water composition was of two types: Ca-Cl and Ca-Na-HCO. The ratio of Cl and δO showed that the Ca-Cl type seepage water was influenced by groundwater mixed with seawater ranging from 2.7% to 15.1%. Various sulfate-reducing bacteria were identified in the Ca-Cl type seepage water, exhibiting relatively high sulfate content from seawater intrusion. Samples from the Ca-Na-HCO type seepage water had an extremely high pH (>10) and abundance of Hydrogenophaga. The precipitates observed along the flow path of the seepage water included calcite, ferrihydrite, green rust, and siderite, depending on seepage water chemistry and microbial activity. This study suggests that the construction of underground structures creates distinct, localized geochemical conditions (e.g., high alkalinity, high salinity, and oxic conditions), which may impact microbial communities. These biogeochemical changes may have undesirable large-scale impacts such as water pump clogging. An understanding of the process and long-term monitoring are essential to assess the safety of underground facilities.
在韩国东海岸的一个地下处理设施附近的两口观测井中,对地下水进行了八年多的监测。结果表明,在设施建设过程中,溶解氧、钠、钙、镁和硫酸盐等离子的浓度显著增加。从筒仓和隧道下游采集了渗漏水样和沿渗流水路径沉积的沉淀物,以确定处理设施内的影响。采用 X 射线分析(粉末 X 射线衍射(pXRD)和 X 射线吸收精细结构(XAFS))对矿物沉淀物进行了表征。通过 16S rRNA 基因测序确定了微生物群落组成。渗漏水的组成有两种类型:Ca-Cl 和 Ca-Na-HCO。Cl 和 δO 的比值表明,Ca-Cl 型渗漏水受到地下水与海水混合的影响,混合比例从 2.7%到 15.1%不等。在 Ca-Cl 型渗漏水中鉴定出各种硫酸盐还原菌,表现出相对较高的硫酸盐含量,来自海水入侵。Ca-Na-HCO 型渗漏水的样品具有极高的 pH 值(>10)和丰富的氢噬菌属。沿渗流水路径观察到的沉淀物包括方解石、水铁矿、绿锈和菱铁矿,这取决于渗漏水的化学性质和微生物活性。本研究表明,地下结构的建设会产生独特的局部地球化学条件(例如,高碱性、高盐度和氧化条件),这可能会影响微生物群落。这些生物地球化学变化可能会产生不良的大规模影响,例如水泵堵塞。了解该过程并进行长期监测对于评估地下设施的安全性至关重要。