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EFFECT OF SORPTION ON BENZENE BIODEGRADATION IN SANDY SOIL

机译:吸附对沙质土壤中生物降解的影响

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The effect of sorption on benzene biodegradation in sandy soil was studied by conducting kinetic microcosm batch tests in soil-free solution and in the presence or absence of bacteria in soil materials with varying degrees of powdered activated carbon (PAC). In the soil-free experiment, benzene was added to a solution inoculated with Pseudomonas aeruginosa bacteria in order to achieve a potential or maximum biodegradation rate. In subsequent experiments, benzene was applied to a solution containing sandy soil and various PAC contents with and without inoculating P. aeruginosa. Benzene concentrations in the soil-free experiments decreased with time with two characteristic rates. A two-stage exponential decay model adequately represented the observed solution concentration pattern with time. Sorption experiments in bacteria-free soil also decreased monotonically, with the extent of sorption increasing as PAC content increased. The sorption data were represented well with a two-stage irreversible sorption model. A third set of experiments in the presence of both soil and bacteria showed more rapid concentration loss from solution than the set of experiments with bacteria-free soil. A model combining sorption and degradation greatly overestimated the loss when the rate coefficient from the bacteria-free experiments was used. Satisfactory agreement between model predictions and observed values was obtained when the degradation rate coefficients were decreased by factors ranging from 3 to 10, depending on the amount of PAC present. Model predictions of the percentage benzene mass remaining in the soil after 25 d of degradation ranged from 72 to 97%, depending on the PAC content, compared to only 2.5% remaining in soil-free solution.
机译:通过在无土壤溶液中进行动力学微观分批测试,以及在土壤中是否存在细菌以及不同程度的粉状活性炭(PAC)的细菌存在下,进行了动力学微观批处理试验,研究了吸附对沙质土壤中苯生物降解的影响。在无土实验中,将苯添加到铜绿假单胞菌细菌接种的溶液中,以实现潜在或最大的生物降解率。在随后的实验中,在接种铜绿假单胞菌和不接种铜绿假单胞菌的情况下,将苯施用到含有沙土和各种PAC含量的溶液中。无土实验中的苯浓度随时间下降,具有两个特征速率。一个两阶段的指数衰减模型可以充分代表所观察到的溶液浓度随时间变化的模式。无菌土壤中的吸附实验也随着PAC含量的增加而单调减少,吸附程度也随之增加。两阶段不可逆吸附模型很好地代表了吸附数据。与没有细菌的土壤相比,在存在土壤和细菌的情况下进行的第三组实验显示溶液中浓度的损失更快。当使用无细菌实验的速率系数时,结合了吸附和降解的模型大大高估了损失。当降解速率系数降低3到10之间时,取决于PAC的存在量,模型预测值与观察值之间就获得了令人满意的一致性。降解25天后,残留在土壤中的苯质量百分比的模型预测范围为PAC的72%至97%,而无土壤溶液中仅残留2.5%。

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