首页> 外文期刊>Journal of Contaminant Hydrology >Effect of injection velocity and particle concentration on transport of nanoscale zero-valent iron and hydraulic conductivity in saturated porous media
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Effect of injection velocity and particle concentration on transport of nanoscale zero-valent iron and hydraulic conductivity in saturated porous media

机译:注入速度和颗粒浓度对纳米零价铁在饱和多孔介质中输运及水力传导率的影响

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Successful groundwater remediation by injecting nanoscale zero-valent iron (NZVI) particles requires efficient particle transportation and distribution in the subsurface. This study focused on the influence of injection velocity and particle concentration on the spatial NZVI particle distribution, the deposition processes and on quantifying the induced decrease in hydraulic conductivity (K) as a result of particle retention by lab tests and numerical simulations. Horizontal column tests of 2 m length were performed with initial Darcy injection velocities (Fe-in(D)) of 0.5, 1.5, and 4.1 m/h and elemental iron input concentrations (Fe-in(0)) of 0.6, 10, and 17 g/L. Concentrations of Fe in the sand were determined by magnetic susceptibility scans, which provide detailed Fe distribution profiles along the column. NZVI particles were transported farther at higher injection velocity and higher input concentrations. K decreased by one order of magnitude during injection in all experiments, with a stronger decrease after reaching Fe-0 concentrations of about 14-18 g/kg (sand). To simulate the observed nanoparticle transport behavior the existing finite-element code OGS has been successfully extended and parameterized for the investigated experiments using blocking, ripening, and straining as governing deposition processes. Considering parameter relationships deduced from single simulations for each experiment (e.g. deposition rate constants as a function of flow velocity) one mean parameter set has been generated reproducing the observations in an adequate way for most cases of the investigated realistic injection conditions. An assessment of the deposition processes related to clogging effects showed that the percentage of retention due to straining and ripening increased during experimental run time resulting in an ongoing reduction of K. Clogging is mainly evoked by straining which dominates particle deposition at higher flow velocities, while blocking and ripening play a significant role for attachment, mainly at lower injection velocities. Since the injection of fluids at real sites leads to descending flow velocities with increasing radial distance from the injection point, the simulation of particle transport requires accounting for all deposition processes mentioned above. Thus, the derived mean parameter set can be used as a basis for quantitative and predictive simulations of particle distributions and clogging effects at both lab and field scale. Since decreases in K can change the flow system, which may have positive as well as negative implications for the in situ remediation technology at a contaminated site, a reliable simulation is thus of great importance for NZVI injection and prediction. (C) 2016 Elsevier B.V. All rights reserved.
机译:通过注入纳米级零价铁(NZVI)颗粒成功地修复地下水,需要在地下进行有效的颗粒运输和分配。这项研究的重点是注射速度和颗粒浓度对空间NZVI颗粒分布,沉积过程的影响,并通过实验室测试和数值模拟量化了由于颗粒保留而导致的导水率(K)降低。在初始Darcy注入速度(Fe-in(D))为0.5、1.5和4.1 m / h且元素铁输入浓度(Fe-in(0))为0.6、10,和17克/升。砂子中的Fe浓度是通过磁化率扫描确定的,该扫描提供了沿柱的详细的Fe分布曲线。 NZVI颗粒在更高的注入速度和更高的输入浓度下被传输得更远。在所有实验中,钾在注射过程中下降了一个数量级,在达到约14-18 g / kg(沙)的Fe-0浓度后,下降幅度更大。为了模拟观察到的纳米粒子的传输行为,现有的有限元代码OGS已成功地扩展和参数化,用于使用阻塞,成熟和应变作为控制沉积过程的研究实验。考虑到从每个实验的单个模拟推导出的参数关系(例如,沉积速率常数作为流速的函数),已经生成了一个平均参数集,可以以足够的方式再现观察到的大多数实际注入条件下的观察结果。对与堵塞效应相关的沉积过程的评估表明,在实验运行期间,由于应变和熟化而导致的保留百分比增加,导致K持续降低。堵塞主要是由应变引起的,应变在较高的流速下占主导地位,而阻塞和成熟对附着起着重要作用,主要是在较低的注射速度下。由于在真实位置注入流体会导致流速下降,并且距注入点的径向距离增加,因此粒子传输的模拟需要考虑上述所有沉积过程。因此,导出的平均参数集可以用作在实验室和现场范围内对颗粒分布和堵塞效应进行定量和预测模拟的基础。由于K的降低会改变流动系统,这可能会对污染场地的原位修复技术产生积极或消极的影响,因此可靠的模拟对于NZVI的注入和预测非常重要。 (C)2016 Elsevier B.V.保留所有权利。

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