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Bacteria transport and retention in intact calcareous soil columns under saturated flow conditions

机译:饱和流条件下完整石灰质土壤中细菌的运输和保留

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摘要

Study of bacterial transport and retention in soil is important for various environmental applications such as groundwater contamination and bioremediation of soil and water. The main objective of this research was to quantitatively assess bacterial transport and deposition under saturated conditions in calcareous soil. A series of leaching experiments was conducted on two undisturbed soil columns. Breakthrough curves of Pseudomonas fluorescens and Cl were measured. After the leaching experiment, spatial distribution of bacteria retention in the soil columns was determined. The HYDRUS-1D one- and two-site kinetic models were used to predict the transport and deposition of bacteria in soil. The results indicated that the two-site model fits the observed data better than one-site kinetic model. Bacteria interaction with the soil of kinetic site 1 revealed relatively fast attachment and slow detachment, whereas attachment to and detachment of bacteria from kinetic site 2 was fast. Fast attachment and slow detachment of site 1 can be attributed to soil calcium carbonate that has favorable attachment sites for bacteria. The detachment rate was less than 0.02 of the attachment rate, indicating irreversible attachment of bacteria. High reduction rate of bacteria was also attributed to soil calcium carbonate.
机译:研究细菌在土壤中的迁移和保留对于各种环境应用至关重要,例如地下水污染以及土壤和水的生物修复。这项研究的主要目的是定量评估石灰性土壤在饱和条件下的细菌迁移和沉积。在两个未扰动的土壤柱上进行了一系列浸出实验。测量了荧光假单胞菌和Cl的穿透曲线。浸出实验后,确定土壤中细菌保留的空间分布。使用HYDRUS-1D一站和两站动力学模型来预测细菌在土壤中的迁移和沉积。结果表明,两点模型比一点动力学模型更好地拟合了观测数据。细菌与动力学位点1的土壤相互作用显示相对较快的附着和较慢的分离,而细菌对动力学位点2的附着和分离则较快。位点1的快速附着和缓慢脱离可以归因于土壤碳酸钙,它对细菌具有有利的附着点。脱离率小于附着率的0.02,表明细菌不可逆地附着。细菌的高还原率也归因于土壤碳酸钙。

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