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Scaling kinetics of organic compounds degradation: laboratory values extended to field sites

机译:有机化合物降解的尺度动力学:实验室值扩展到现场

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In this paper we study the degradation kinetics of chlorinated solvents in the laboratory and in the field. Microcosms were prepared from groundwater from a field site and showed biodegradation of PCE to ethene only when organic matter (as propionate) was added to the microcosm. In the field, the same geochemical model was applied in conjunction with a transport model to simulate chlorinated solvents and electron acceptors concentrations. Due to the uncertainty on the size of the degradation zone (reducing area) several values of kinetic constant and several models might be used to fit the measured field data. A model using kinetic values obtained in the laboratory suggests that degradation only occurs in a small area. From this study and data from other sites, two major conclusions can be drawn: (i) at most sites the area where degradation occurs seems to be fairly small, and (ii) for chlorinated solvents plume modelling, working on electron acceptors spatial distribution is as important as assessing the kinetic degradation rates.
机译:在本文中,我们在实验室和现场研究了氯化溶剂的降解动力学。从野外的地下水中制备了微观世界,只有在将有机物(作为丙酸酯)添加到微观世界中时,PCE才会生物降解为乙烯。在野外,将相同的地球化学模型与运输模型结合使用,以模拟氯化溶剂和电子受体的浓度。由于降解区(还原区)大小的不确定性,可以使用动力学常数的几个值和几个模型来拟合实测数据。使用实验室获得的动力学值的模型表明,降解仅发生在很小的区域。从这项研究和其他站点的数据中,可以得出两个主要结论:(i)在大多数站点上,发生降解的区域似乎很小,(ii)对于氯化溶剂羽流模型,研究电子受体的空间分布是与评估动力学降解速率一样重要。

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