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Identification of TCE and PCE sorption and biodegradation parameters in a sandy aquifer for fate and transport modelling: batch and column studies

机译:鉴定砂质含水层中TCE和PCE的吸附和生物降解参数以进行命运和运输建模:分批和色谱柱研究

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摘要

The main aim of this study was to determine the sorption and biodegradation parameters of trichloroethene (TCE) and tetrachloroethene (PCE) as input data required for their fate and transport modelling in a Quaternary sandy aquifer. Sorption was determined based on batch and column experiments, while biodegradation was investigated using the compound-specific isotope analysis (CSIA). The aquifer materials medium (soil 1) to fine (soil 2) sands and groundwater samples came from the representative profile of the contaminated site (south-east Poland). The sorption isotherms were approximately linear (TCE, soil 1, Kd = 0.0016; PCE, soil 1, Kd = 0.0051; PCE, soil 2, Kd = 0.0069) except for one case in which the best fitting was for the Langmuir isotherm (TCE, soil 2, Kf = 0.6493 and Smax = 0.0145). The results indicate low retardation coefficients (R) of TCE and PCE; however, somewhat lower values were obtained in batch compared to column experiments. In the column experiments with the presence of both contaminants, TCE influenced sorption of PCE, so that the R values for both compounds were almost two times higher. Non-significant differences in isotope compositions of TCE and PCE measured in the observation points (δ13C values within the range of −23.6 ÷ −24.3 ‰ and −26.3 ÷−27.7 ‰, respectively) indicate that biodegradation apparently is not an important process contributing to the natural attenuation of these contaminants in the studied sandy aquifer.
机译:这项研究的主要目的是确定三氯乙烯(TCE)和四氯乙烯(PCE)的吸附和生物降解参数,作为它们在第四纪含砂含水层中的命运和运移模型所需的输入数据。根据批次和色谱柱实验确定吸附,同时使用化合物特异性同位素分析(CSIA)研究生物降解。含水层材料介质(土壤1)至细砂(土壤2)和地下水样品来自受污染场地(波兰东南部)的代表性剖面。吸附等温线近似线性(TCE,土壤1,Kd = 0.0016; PCE,土壤1,Kd = 0.0051; PCE,土壤2,Kd = 0.0069),其中一种情况最适合Langmuir等温线(TCE)。 ,土壤2,Kf = 0.6493和Smax = 0.0145)。结果表明,TCE和PCE的延迟系数(R)低;但是,与色谱柱实验相比,分批获得的值较低。在同时存在两种污染物的色谱柱实验中,TCE影响了PCE的吸附,因此两种化合物的R值几乎高出两倍。在观测点测得的TCE和PCE同位素组成的无显着差异(δ 13 C值分别在-23.6÷-24.3‰和-26.3÷-27.7−‰范围内)表明:生物降解显然不是一个重要的过程,它有助于研究的含沙含水层中这些污染物的自然衰减。

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