非水相液体污染场地的地球物理特征

Q2 Earth and Planetary Sciences Environmental Geosciences Pub Date : 2010-12-01 DOI:10.1306/EG.04261010003
A. Godio, A. Arato, S. Stocco
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引用次数: 14

摘要

采用地球物理方法对土壤和地下水被非水相液体(NAPL)污染的场地进行了表征;碳氢化合物在地下水位以上以残余形式和自由相存在。地球物理调查的目的是提高对场址水文地质环境的认识;我们想要估计土壤的异质性和水文地质参数(孔隙度、含水量和水力传导性)。我们还想评估地下水位波动对地下水与剩余NAPL之间相互作用的影响。地球物理调查采用地电、电磁(频域)和地质雷达方法;利用井眼地球化学测井资料进行数据校准。在粉质和砂质材料中残留NAPL的存在,可以通过震波能量衰减的显著增加和诱导极化响应的峰值来证实。在水深5米(15英尺)处检测到的碳氢化合物浓度超过1000 mg/kg (1000 ppm),在水深6至8米(18-24英尺)处检测到的碳氢化合物浓度为3000 mg/kg (3000 ppm)。
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Geophysical characterization of a nonaqueous-phase liquid–contaminated site
Geophysical methods have been adopted to characterize a site whose soils and groundwater had been contaminated by nonaqueous-phase liquid (NAPL); the hydrocarbons were found in both residual form and as a free phase above the water table. The geophysical survey was aimed at improving the knowledge of the hydrogeological setting of the site; we wanted to estimate the soil heterogeneity and the hydrogeological parameters (porosity, water content, and hydraulic conductivity). We also wanted to assess the effect of the water table fluctuations on the interaction between the groundwater and the residual NAPL. The geophysical investigation was conducted using geoelectrical, electromagnetic (frequency domain), and georadar methods; data calibration was conducted using borehole geochemical logs. The presence of residual NAPL in the silty and sandy material was confirmed by a remarkable increase of the attenuation in the georadar energy and by peak of induced polarization response. The hydrocarbons have been detected in concentrations of more than 1000 mg/kg (1000 ppm) at a depth of 5 m (15 ft) and in concentrations of 3000 mg/kg (3000 ppm) at a depth of 6 to 8 m (18–24 ft).
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Environmental Geosciences
Environmental Geosciences Earth and Planetary Sciences-Earth and Planetary Sciences (all)
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