首页> 外文会议>2009 ISEST;International symposium on environmental science and technology >Use the Electrical Resitivity Image as a Non-Invasive Method to Study the Characterization of Landfills
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Use the Electrical Resitivity Image as a Non-Invasive Method to Study the Characterization of Landfills

机译:使用电阻率图像作为非侵入性方法来研究垃圾掩埋场的特征

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Electrical resistivity imaging is used increasingly as a geophysical exploration technique in contaminated land research. The presented work demonstrates the efficiency of electrical imaging in monitoring pollution plume evolution under the landfill and geological mapping around the landfill, employing electrical resistivity and time domain induced polarization (IP) methods. Nine electrical resistivity imaging (ERI) surveys were conducted in the summer of 2005, in which five surveys around the landfill mapped the geology and four on the landfill mapped the leachate distribution. The ERI survey coupled with ground truthing by borehole logging revealed the geology around the landfill has a clay layer varying 5 to 20 m followed by a sand zone with a varying thickness of 5 to 40 m, followed by till. The ERI conducted north and south of the landfill indicated the presence of large areas of leachate accumulation with low resistivity values of less than 8 m and IP values greater than 20 mV/V measured in terms of chargeability. The ERI profile conducted at the north top of the landfill mapped the presence of a high resistive zone at 30 m below the surface, possibly due to the high organic load of the backfilled oil disposal pit.
机译:电阻率成像越来越多地用作污染土地研究中的地球物理勘探技术。提出的工作证明了利用电阻率和时域感应极化(IP)方法,电子成像可以有效监测垃圾填埋场下的污染羽流演变以及垃圾填埋场周围的地质图。 2005年夏天进行了9次电阻率成像(ERI)调查,其中,在垃圾填埋场周围进行了五次调查,绘制了地质图,在垃圾填埋场进行了四次调查,测出了渗滤液分布。 ERI调查加上通过钻孔测井进行的地面实测显示,垃圾填埋场周围的地质层的黏土层变化范围为5至20 m,随后是厚度变化为5至40 m的砂层,最后是直到。在填埋场的北部和南部进行的ERI表明存在大面积的渗滤液积聚,其低电阻率值小于8 m,IP值大于20 mV / V(以可充电性衡量)。在填埋场北端进行的ERI剖面图表明,在地表以下30 m处存在高电阻区,这可能是由于回填的油处理坑的有机负荷较高所致。

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