Detecting subsurface contamination using ground penetrating radar and amplitude variation with offset analysis

E. Babcock, J. Bradford
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引用次数: 8

Abstract

Characterization of contamination in the subsurface is expensive, difficult, and often unreliable. Characterizing Dense Non-Aqueous Phase Liquid (DNAPL) contamination is especially difficult. Geophysical methods, including ground penetrating radar (GPR), are well-suited to measurement of NAPL contamination, as they offer the potential to detect isolated contaminant distributions that borehole monitoring or other methods may miss. We measure the Amplitude Variation with Offset (AVO) response of radar energy to a chlorinated solvent (3M Novec HFE-7200) in a laboratory experiment through controlled injections of the 7200 fluid into a saturated sand/clay system. We demonstrate well defined AVO anomalies associated with the simulate DNAPL spill. The experiment shows that AVO anomalies can be induced when the contaminant layer is as thin as 1/30 the wavelength of the signal at the dominant frequency.
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用探地雷达探测地下污染,用偏移量分析振幅变化
表征地下污染是昂贵的,困难的,而且往往是不可靠的。表征致密非水相液体(DNAPL)污染尤其困难。包括探地雷达(GPR)在内的地球物理方法非常适合测量NAPL污染,因为它们有可能检测到井眼监测或其他方法可能遗漏的孤立污染物分布。我们在实验室实验中,通过将7200流体受控注入饱和砂/粘土系统,测量了雷达能量对氯化溶剂(3M Novec HFE-7200)的偏移响应振幅变化(AVO)。我们展示了与模拟DNAPL泄漏相关的良好定义的AVO异常。实验表明,当污染层薄至占主导频率信号波长的1/30时,可以诱发AVO异常。
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