Dipartimento di Scienze, Università degli Studi Roma Tre, Largo San Leonardo Murialdo 1, 00146, Rome, Italy.
Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur, West Bengal, 721302, India.
Environ Sci Pollut Res Int. 2018 May;25(13):12515-12527. doi: 10.1007/s11356-018-1429-0. Epub 2018 Feb 20.
Geochemical and geophysical surveys employing radon deficit, resistivity, and induced polarization (IP) measurements were undertaken on soil contaminated with non-aqueous phase liquids (NAPLs) in two different sites in India and in Italy. Radon deficit, validated through the comparison with average soil radon in reference unpolluted areas, shows the extension of contamination in the upper part of the unsaturated aquifers. In site 1 (Italy), the spill is not recent. A residual film of kerosene covers soil grains, inhibiting their chargeability and reducing electrical resistivity difference with background unpolluted areas. No correlation between the two parameters is observed. Soil volatile organic compounds (VOCs) concentration is not linked with radon deficit, supporting the old age of the spillage. NAPL pollution in sites 2a and 2b (India) is more recent and probably still active, as demonstrated by higher values of electrical resistivity. A good correlation with IP values suggests that NAPL is still distributed as droplets or as a continuous phase in the pores, strengthening the scenario of a fresh spill or leakage. Residual fraction of gasoline in the pore space of sites 2a and 2b is respectively 1.5 and 11.8 kg per cubic meter of terrain. This estimation is referred to the shallower portion of the unsaturated aquifer. Electrical resistivity is still very high indicating that the gasoline has not been strongly degraded yet. Temperature and soil water content influence differently radon deficit in the three areas, reducing soil radon concentration and partly masking the deficit in sites 2a and 2b.
在印度和意大利的两个不同地点,对受非水相液体(NAPL)污染的土壤进行了地球化学和地球物理调查,采用了氡亏缺、电阻率和激发极化(IP)测量。氡亏缺通过与参考未污染地区的平均土壤氡进行比较得到验证,显示了非饱和含水层上部污染的延伸。在地点 1(意大利),泄漏不是最近的。一层残留的煤油覆盖在土壤颗粒上,抑制了它们的荷电性,并降低了与背景未污染地区的电阻率差异。这两个参数之间没有相关性。土壤挥发性有机化合物(VOC)浓度与氡亏缺无关,支持泄漏的年代久远。地点 2a 和 2b(印度)的 NAPL 污染更新近,可能仍然活跃,这反映在更高的电阻率值上。与 IP 值的良好相关性表明,NAPL 仍然以液滴或连续相的形式分布在孔隙中,强化了新的溢出或泄漏的情景。地点 2a 和 2b 孔隙空间中残留的汽油分别为每立方米 1.5 和 11.8 公斤。这一估计是指非饱和含水层较浅的部分。电阻率仍然非常高,表明汽油尚未强烈降解。温度和土壤含水量对三个地区的氡亏缺有不同的影响,降低了土壤氡浓度,并在一定程度上掩盖了地点 2a 和 2b 的亏缺。