Squillace Paul J, Moran Michael J
U.S. Geological Survey, 1608 Mountain View Road, Rapid City, South Dakota 57702, USA.
Environ Sci Technol. 2007 Apr 1;41(7):2123-30. doi: 10.1021/es061079w.
Factors associated with sources, transport, and fate of volatile organic compounds (VOCs) in groundwater from aquifers throughout the United States were evaluated using statistical methods. Samples were collected from 1631 wells throughout the conterminous United States between 1996 and 2002 as part of the National Water-Quality Assessment (NAWQA) Program of the U.S. Geological Survey. Water samples from wells completed in aquifers used to supply drinking water were analyzed for more than 50 VOCs. Wells were primarily rural domestic water supplies (1184), followed by public water supplies (216); the remaining wells (231) supplied a variety of uses. The median well depth was 50 meters. Age-date information shows that about 60% of the samples had a fraction of water recharged after 1953. Chloroform, toluene, 1,2,4-trimethyl-benzene, and perchloroethene were some of the frequently detected VOCs. Concentrations generally were less than 1 microg/L. Source factors include, in order of importance, general land-use activity, septic/sewer density, and sites where large concentrations of VOCs are potentially released, such as leaking underground storage tanks. About 10% of all samples had VOC mixtures that were associated with concentrated sources; 20% were associated with dispersed sources. Important transport factors included well/screen depth, precipitation/groundwater recharge, air temperature, and various soil characteristics. Dissolved oxygen was strongly associated with VOCs and represents the fate of many VOCs in groundwater. Well type (domestic or public water supply) was also an important explanatory factor. Results of multiple analyses show the importance of (1) accounting for both dispersed and concentrated sources of VOCs, (2) measuring dissolved oxygen when sampling wells to help explain the fate of VOCs, and (3) limiting the type of wells sampled in monitoring networks to avoid unnecessary variance in the data, or controlling for this variance during data analysis.
利用统计方法对美国各地含水层地下水中挥发性有机化合物(VOCs)的来源、迁移和归宿相关因素进行了评估。作为美国地质调查局国家水质评估(NAWQA)计划的一部分,1996年至2002年期间从美国本土1631口井采集了样本。对用于供应饮用水的含水层中完成的井的水样进行了50多种挥发性有机化合物的分析。这些井主要是农村家庭供水井(1184口),其次是公共供水井(216口);其余的井(231口)用于多种用途。井的中位深度为50米。年代测定信息表明,约60%的样本有一部分水是1953年以后补给的。氯仿、甲苯、1,2,4-三甲基苯和全氯乙烯是一些经常检测到的挥发性有机化合物。浓度一般低于1微克/升。来源因素按重要性排序包括一般土地利用活动、化粪池/下水道密度以及挥发性有机化合物可能大量释放的场所,如地下储油罐泄漏处。所有样本中约10%的挥发性有机化合物混合物与集中源有关;20%与分散源有关。重要的迁移因素包括井/滤网深度、降水/地下水补给、气温和各种土壤特性。溶解氧与挥发性有机化合物密切相关,代表了许多挥发性有机化合物在地下水中的归宿。井的类型(家庭或公共供水)也是一个重要的解释因素。多重分析结果表明:(1)考虑挥发性有机化合物的分散源和集中源;(2)在对井进行采样时测量溶解氧以帮助解释挥发性有机化合物的归宿;(3)限制监测网络中采样井的类型以避免数据中出现不必要的差异,或在数据分析过程中控制这种差异,这些都很重要。