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TDR detection of nonaqueous phase liquids in sandy soils using the eigendecomposition method

机译:本征分解法对砂质土壤中非水相液体进行TDR检测

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In this study, the presence of nonaqueous phase liquids (NAPL) in sandy soils are detected using a TDR probe system and the eigendecomposition method of analysis. As a demonstration, five NAPLs with different physicochemical properties (acetone, benzene, heptane, trichloroethylene, and xylene; Table 1) were used. Samples were prepared in such a way that the soil pore fluid has different contents of deionized water and NAPLs. For each experiment, a pulse signal with known characteristics was used and reflected signals were captured by an oscilloscope and analyzed using the eigendecomposition method. Autoregressive modeling and singular value decomposition were used to calculate the eigenvalues. The most significant eigenvalues were identified based on their power spectrum. The relative eigenvalue of the first mode (Eow), which is a measure of the power carried by the signal, was calculated and correlated to NAPL type and content, and octanol water partition coefficient (log Kow). The results indicated that for the same NAPL content, as log Kow increases, Eow decreases due to increase of hydrophobicity. For the same log Kow, as the organic content in soil pore fluid increases, Eow increases due to decrease of dielectric properties of the pore fluids.
机译:在这项研究中,使用TDR探针系统和特征分解法检测沙质土壤中非水相液体(NAPL)的存在。作为演示,使用了五个具有不同理化性质的NAPL(丙酮,苯,庚烷,三氯乙烯和二甲苯;表1)。样品的制备应使土壤孔隙液中的去离子水和NAPL含量不同。对于每个实验,均使用具有已知特征的脉冲信号,并通过示波器捕获反射信号并使用特征分解法进行分析。使用自回归建模和奇异值分解来计算特征值。根据其功率谱确定了最重要的特征值。计算出第一模式的相对特征值(Eow),它是信号所承载功率的度量,并与NAPL类型和含量以及辛醇水分配系数(log Kow)相关。结果表明,对于相同的NAPL含量,随着log Kow的增加,Eow因疏水性的增加而降低。对于相同的log Kow,随着土壤孔隙液中有机物含量的增加,Eow会由于孔隙液介电性能的降低而增加。

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