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Groundwater contamination with petroleum hydrocarbons, chlorinated solvents and high pH: implications for multiple sources

机译:石油碳氢化合物,氯化溶剂和高pH值对地下水的污染:对多种来源的影响

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摘要

Groundwater was contaminated with petroleum hydrocarbons (toluene and xylenes) and chlorinated solvents (PCE, TCE) at a Korean national groundwater monitoring station (NGMS). The shallow groundwater was also very alkaline (pH 11–12) with a very high electrical conductivity (EC) of over 3000 µS cm–1. Extensive diagnostic investigation of potential contamination sources and groundwater and stream water quality for the whole surrounding area revealed that the groundwater contamination was spatially restricted to a small area of the monitoring station. Detailed investigation of the small area uncovered the existence of many waste asphalt emulsion containers and various road construction waste materials within a 15 m distance from the monitoring station. All relevant diagnostic and detailed investigation results, including contamination history (coincidence of road construction period with contamination period), vertical EC distribution and surrounding groundwater and stream water quality, indicated that the shallow groundwater contamination of the NGMS was caused by illegal dumping of the road construction waste on the surface at the site. A pulse input of liquid waste containing solvents and petroleum hydrocarbons is suspected as the most plausible cause for the contamination. Sustained high pH of groundwater indicates the possible existence of raw cement product in the subsurface, which requires further investigation.
机译:在韩国国家地下水监测站(NGMS)中,地下水被石油烃(甲苯和二甲苯)和氯化溶剂(PCE,TCE)污染。浅层 地下水也很碱性(pH 11–12),非常 高电导率(EC)超过3000 µS cm –1 对整个 周边地区潜在污染源和地下水以及溪流水水质的广泛诊断研究表明,地下水污染 在空间上仅限于监测站的一小部分。 对该小区域的详细调查发现, 存在许多废沥青乳液容器和各种道路建设 在距监测站15 m的范围内浪费材料。 所有相关的诊断和详细调查结果, 包括污染历史(道路建设巧合 < / sup>带有污染期的时期),垂直EC分布 以及周围的地下水和溪流水质,以 表示NGMS的浅层地下水污染是由 造成的,这是由于道路施工废料被非法倾倒在现场的表面上。脉冲输入包含溶剂 和石油碳氢化合物的液体废物被认为是造成污染的最可能的 原因。地下水的高pH值 表示 地下可能存在水泥原料,这需要进一步研究。

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    Department of Geology, Kangwon National University, Chuncheon 200-701, South Korea, Republic of Korea(hydrolee@kangwon.ac.kr);

    Groundwater & Geothermal Resources Division, KIGAM, Daejeon 305-350, South Korea, Republic of Korea;

    GeoGreen21 Co., Ltd., Suite 901, E&C Venture Dream Tower II, 197-10, Guro-dong, Seoul 152-050,South Korea, Republic of Korea;

    Department of Earth and Environmental Sciences, Korea University, Seoul 136-701, South Korea,Republic of Korea;

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