Fluctuation of Citrobacter Transport Influenced by High Porous Medium in Homogeneous Silty Formation in Saline Environment

Eluozo Sn, Ogbonda C
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Abstract

This paper monitor the deposition of Citrobacter in high porous medium in saline environment, the study investigate the behaviour of the contaminant in saline environment, the application of deterministic model developed simulation values that express the behaviour and effect from high porous medium, such shallow phreatic bed were observed to experiences fluctuation in soil porosity thus reflecting on the rate of concentration. The simulation developed locations that the concentration generated fluctuation to the depth were it was in significant in the formation, this was observed to be in an area were Citrobacter experiences degradation due to lack of microelement for growth. Moreso its deposition in shallow Phreatic zone has evaluated the rate of transport with respect to time and depth from the study carried out, it was observed to be predominantly influenced by high porosity in the formation, the influences of alluvium deposit in these condition could not influences the aquiferous zone by uniformity of the Phreatic deposited strata. Formation characteristics stated above were found significant in the migration of Citrobacter from surface to phreatic zone. The models were simulated and it produced theoretical values compared with other measured results, both parameters developed a favuorable fits validating the model.
盐渍环境下均匀粉砂质地层中高孔隙介质对柠檬酸杆菌迁移的影响
本文对盐渍环境中高孔隙介质中柠檬酸杆菌的沉积进行了监测,研究了盐渍环境中柠檬酸杆菌的行为,应用确定性模型建立了表征高孔隙介质中柠檬酸杆菌行为和影响的模拟值,观察到浅埋层土壤孔隙度的波动,从而反映了浓度的变化速率。模拟发现了地层中浓度产生深度波动的位置,观察到这是由于缺乏生长所需的微量元素而导致柠檬酸杆菌降解的区域。此外,对其在浅层潜水带的沉积进行了随时间和深度的运移速率评价,观察到其主要受地层高孔隙度的影响,冲积层在这些条件下的影响不能通过潜水沉积地层的均匀性来影响含水带。上述形成特征在柠檬酸杆菌从表面向潜水带迁移过程中具有重要意义。对模型进行了仿真,并与其他实测结果进行了比较,得到了理论值,两个参数拟合良好,验证了模型的正确性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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