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Tracing sources of natural organic matter, trihalomethanes and metals in groundwater from a karst region

机译:喀斯特地区地下水中的天然有机物,三卤代甲烷和金属的追踪来源

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摘要

Groundwater offers an important source for drinking water around the world; however, groundwater quality is under increasing pressure and is particularly vulnerable in karst areas. Total organic carbon (TOC) is significantly related to groundwater quality and when not removed by water treatment processes can give rise to the formation of disinfection by-products trihalomethanes (THMs) above the level of compliance. This study investigated the source of organic matter giving rise to the THM exceedances in a groundwater supply in a karst area. Results highlighted?that?source water?for this groundwater supply was prone to surface water infiltration linked to rainfall events; was not accurately captured in the zone of contribution (ZoC); had inadequate treatment of natural organic matter (NOM) and suffered THM exceedances in 45% of sampling events. THMs were mostly represented by chloroform and caused by terrestrial delivered reprocessed organic matter. This work will support water managers tasked with decision-making.
机译:地下水为世界各地饮用水提供了重要的来源;然而,地下水质量处于越来越大的压力,并且在喀斯特地区尤其脆弱。总有机碳(TOC)与地下水质量显着相关,并且当不通过水处理过程中除去时可以产生副产物的消毒副产物三卤代甲烷(THM)以上的顺从程度。本研究调查了在喀斯特地区的地下水供应中产生了有机质的来源。结果突出显示?源水?对于这种地下水供应,易于表面水渗透与降雨事件有关;在贡献区域(ZOC)没有准确捕获;在治疗天然有机物(NOM)的治疗不足,并且在45%的抽样事件中遭受了足够的影响。 THM大多由氯仿代表,并由陆地传递后处理的有机物引起。这项工作将支持有关决策的水管理者。

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