首页> 外文会议>3rd British Geotechnical Association Geoenvironmental Engineering Conference Sep 17-19, 2001 Edinburgh, Scotland >The influence of fluctuations in the groundwater table on Monitored Natural Attenuation
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The influence of fluctuations in the groundwater table on Monitored Natural Attenuation

机译:地下水位波动对监测自然衰减的影响

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Because of the interaction between the dissolution of components and the distribution of the residual NAPL-phase in the pores multiphase-fluid flow and the contaminant transport have to be investigated considering the effect of hysteresis. The natural processes are influenced by the interactions between the air-, water- und contaminant phase, e.g. by changing supply of molecular oxygen. The solubility of organic compounds varies due to time the groundwater stays inside the contaminated area, as well. Summarising a remediation by Monitored Natural Attenuation requires the following site characterization information: 1. Laboratory and field investigation of soil mechanical and chemical properties of the soil and of the hydrological, chemical and biological properties of the fluids e.g. locations of potential receptors, direction of ground water flow and hydraulic conductivity. 2. Modelling of the processes running in the soil and groundwater. 3. Validation of the numerical processes by small and large model tests in the laboratory and in-situ and evaluation remedial processes. 4. Appropriate monitoring program, based on the principals of the observational method, which is a well known and successful in classic soil mechanical approach (deep excavations, slopes, tunnelling, high loaded foundations. 5. Checking the estimated natural processes. However the interaction between the multiphase-fluid flow and contaminant transport have to be considered to estimate the effectiveness of natural attenuation.
机译:由于组分的溶解与孔隙中残留NAPL相的分布之间存在相互作用,因此必须考虑滞后效应,研究多相流体流动和污染物的运移。自然过程受空气,水和污染物相之间相互作用的影响,例如通过改变分子氧的供应。有机化合物的溶解度也会因地下水停留在受污染区域内的时间而变化。总结通过监测的自然衰减进行的补救需要以下现场特征信息:1.对土壤的土壤机械和化学特性以及流体的水文,化学和生物学特性(例如土壤)进行实验室和现场调查。潜在受体的位置,地下水流向和水力传导率。 2.对在土壤和地下水中运行的过程进行建模。 3.通过实验室中的小型和大型模型测试以及现场和评估补救过程来验证数值过程。 4.基于观测方法原理的适当监测程序,在经典的土壤力学方法(深基坑,斜坡,隧道,高荷载地基中)是众所周知的且成功的方法。5.检查估计的自然过程。为了估计自然衰减的有效性,必须考虑多相流体流动与污染物运移之间的关系。

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