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Transport and deposition of sediment-associated Escherichia coli in natural streams

机译:沉积物相关大肠杆菌在自然流中的运输和沉积

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The association of microorganisms with sediment particles is one of the primary complicating factors in assessing microbial fate in aquatic systems. The literature indicates that the majority of enteric bacteria in aquatic systems are associated with sediments and that these associations influence their survival and transport characteristics. Yet, the nature of these associations has not been fully characterized. In this study, a combination of field experiments and mathematical modeling were used to better understand the processes which control the fate and transport of enteric bacteria in alluvial streams. An experimental procedure, involving the use of a tracer-bacteria, was developed to simulate the transport and deposition of bacteria-laden bed sediments in a small alluvial stream during steady flow conditions. The experimental data and mathematical model were used to determine dispersion coefficients, deposition rates, and partitioning coefficients for sediment-associated bacteria in two natural streams. The results provided evidence that bacterial adsorption can be modeled as an irreversible process in freshwater environments. Net settling velocities of fine sediments and associated bacteria were typically two orders of magnitude lower than those predicted from Stokes equation, due to re-entrainment of settled particles. The information presented in this study will further the development of representative microbial water quality models.
机译:微生物与沉积物颗粒的结合是评估水生系统中微生物命运的主要复杂因素之一。文献表明,水生系统中的大多数肠细菌与沉积物有关,并且这些结合会影响其生存和运输特性。但是,这些协会的性质尚未得到充分表征。在这项研究中,结合了野外实验和数学模型来更好地了解控制冲积流中肠细菌命运和运输的过程。开发了一种实验方法,其中涉及使用示踪细菌,以模拟在稳定流动条件下小冲积流中载有细菌的床沉积物的运输和沉积。实验数据和数学模型用于确定两种自然流中与沉积物相关的细菌的分散系数,沉积速率和分配系数。结果提供了证据,表明细菌吸附可以被建模为淡水环境中的不可逆过程。细颗粒沉积物和相关细菌的净沉降速度通常比斯托克斯方程预测的要低两个数量级,这是由于沉降颗粒的重新夹带。本研究中提供的信息将进一步发展代表性的微生物水质模型。

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