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NATURAL ATTENUATION AS THE CORRECTIVE ACTION FOR LANDFILL GAS EFFECTS ON GROUNDWATER

机译:自然衰减作为填埋气对地下水的正作用

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Detections of volatile organic compounds (VOCs) in groundwater samples from a monitoring well located downgradient of the Forster Canyon Landfill led to an investigation. The objectives of the investigation were to evaluate the source of the VOCs in the groundwater (landfill gas or landfill leachate) and the extent of VOC-impacted groundwater. Landfill gas was suspected as the source of the VOC detections in the groundwater based on methane concentrations in the headspace of this well and based on the absence of semi-VOCs and other organic compounds in the groundwater samples. Historical groundwater data for this well were evaluated and it was found that increases in VOC concentrations were not accompanied by increases in sodium or chloride concentrations, ruling out a leachate source for the VOC detections. The stratigraphy around the well includes a sand lens in the unsaturated zone, approximately 5-feet thick, which is overlain and underlain by silt and clay layers. Pressure-driven landfill gas transport through the unsaturated sand lens directly into the well was suspected as the process by which the landfill gas affected groundwater. This "in-well" landfill gas effect was evaluated during the investigation. The monitoring well headspace gas and groundwater VOC concentrations were compared and it was found that the direction of the concentration gradient was consistent with landfill gas-to-groundwater transport of the VOCs. Fate and transport modeling of the VOCs in the groundwater phase was then performed using the US EPA model BIOSCREEN for natural attenuation. Because of the limited area of the in-well landfill gas effects, modeling results indicated that VOC concentrations decrease by natural attenuation to regulatory drinking water standards and to laboratory method detection limits within 135 ft of the impacted well. Because the distance to the closest potential receptor is over 3,000 ft natural attenuation was found to be an adequate corrective action for the VOC plume.
机译:从位于福斯特峡谷填埋场下坡的监测井中检测到的地下水样品中的挥发性有机化合物(VOC)引起了调查。研究的目的是评估地下水(垃圾填埋气或垃圾渗滤液)中挥发性有机化合物的来源以及挥发性有机化合物对地下水的影响程度。根据该井顶部空间的甲烷浓度以及地下水样品中不存在半挥发性有机化合物和其他有机化合物的情况,怀疑填埋气是地下水中VOC的检测来源。对这口井的历史地下水数据进行了评估,发现VOC浓度的增加并没有伴随钠或氯化物浓度的增加,从而排除了用于VOC检测的渗滤液源。井周围的地层在不饱和区中有一个沙透镜,厚约5英尺,它被粉砂和粘土层覆盖和覆盖。压力驱动的垃圾填埋气通过不饱和砂粒直接进入井中,被认为是垃圾填埋气影响地下水的过程。在调查过程中评估了这种“井内”垃圾填埋气体的影响。比较了监测井顶空气体和地下水中VOC的浓度,发现浓度梯度的方向与VOC的填埋气向地下水的运移方向一致。然后使用美国EPA模型BIOSCREEN对地下水中的VOC进行去向和迁移建模,以实现自然衰减。由于井内填埋气体影响的区域有限,建模结果表明,VOC浓度会因自然衰减而降低,达到法规饮用水标准和受影响井135英尺内的实验室方法检测极限。因为到最接近的潜在受体的距离超过3,000英尺,所以发现自然衰减是对VOC羽流的适当纠正措施。

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