US Geological Survey, South Carolina Water Science Center, 720 Gracern Road, Suite 129, Columbia, SC 29210, USA.
Ground Water. 2010 Jan-Feb;48(1):30-41. doi: 10.1111/j.1745-6584.2009.00608.x. Epub 2009 Jul 31.
Groundwater contamination by fuel-related compounds such as the fuel oxygenates methyl tert-butyl ether (MTBE), tert-butyl alcohol (TBA), and tert-amyl methyl ether (TAME) presents a significant issue to managers and consumers of groundwater and surface water that receives groundwater discharge. Four sites were investigated on Long Island, New York, characterized by groundwater contaminated with gasoline and fuel oxygenates that ultimately discharge to fresh, brackish, or saline surface water. For each site, contaminated groundwater discharge zones were delineated using pore water geochemistry data from 15 feet (4.5 m) beneath the bottom of the surface water body in the hyporheic zone and seepage-meter tests were conducted to measure discharge rates. These data when combined indicate that MTBE, TBA, and TAME concentrations in groundwater discharge in a 5-foot (1.5-m) thick section of the hyporheic zone were attenuated between 34% and 95%, in contrast to immeasurable attenuation in the shallow aquifer during contaminant transport between 0.1 and 1.5 miles (0.1 to 2.4 km). The attenuation observed in the hyporheic zone occurred primarily by physical processes such as mixing of groundwater and surface water. Biodegradation also occurred as confirmed in laboratory microcosms by the mineralization of U- (14)C-MTBE and U-(14)C-TBA to (14)CO(2) and the novel biodegradation of U- (14)C-TAME to (14)CO(2) under oxic and anoxic conditions. The implication of fuel oxygenate attenuation observed in diverse hyporheic zones suggests an assessment of the hyporheic zone attenuation potential (HZAP) merits inclusion as part of site assessment strategies associated with monitored or engineered attenuation.
受燃料相关化合物(如燃料含氧化合物甲基叔丁基醚 (MTBE)、叔丁醇 (TBA) 和叔戊基甲基醚 (TAME))污染的地下水对地下水和接受地下水排放的地表水的管理者和消费者构成了重大问题。在纽约长岛调查了四个地点,这些地点的地下水受到汽油和燃料含氧化合物的污染,最终排放到淡水、微咸水或咸地表水。对于每个地点,使用位于地表水底部下方 15 英尺(4.5 米)的孔隙水地球化学数据来划定受污染的地下水排放区,并进行渗流计测试以测量排放速率。这些数据表明,在 5 英尺(1.5 米)厚的近地表带中,地下水排放中的 MTBE、TBA 和 TAME 浓度在地下带中衰减了 34%至 95%,而在污染物运移期间,浅层含水层中几乎没有衰减 0.1 至 1.5 英里(0.1 至 2.4 公里)。在近地表带中观察到的衰减主要是通过物理过程发生的,例如地下水和地表水的混合。在实验室微宇宙中也发生了生物降解,这一点通过 U-(14)C-MTBE 和 U-(14)C-TBA 矿化生成 (14)CO(2) 以及在好氧和缺氧条件下新型 U-(14)C-TAME 生物降解生成 (14)CO(2) 得到证实。在不同的近地表带中观察到的燃料含氧化合物衰减的影响表明,评估近地表带衰减潜力 (HZAP) 值得作为与监测或工程衰减相关的场地评估策略的一部分进行评估。