Toloni Ivan, Lehmann François, Ackerer Philippe
LHyGeS, Université de Strasbourg/EOST - CNRS, 1 rue Blessig, 67084 Strasbourg Cedex, France.
LHyGeS, Université de Strasbourg/EOST - CNRS, 1 rue Blessig, 67084 Strasbourg Cedex, France.
J Contam Hydrol. 2016 Aug;191:76-87. doi: 10.1016/j.jconhyd.2016.05.006. Epub 2016 May 31.
The transport of manufactured titanium dioxide (TiO2, rutile) nanoparticles (NP) in porous media was investigated by metric scale column experiments under different water saturation and ionic strength (IS) conditions. The NP breakthrough curves showed that TiO2 NP retention on the interface between air and water (AWI) and the interface between the solid and the fluid (SWI) is insignificant for an IS equal to or smaller than 3mM KCl. For larger IS, the retention is depending on the water content and the fluid velocity. The experiments, conducted with an IS of 5mM KCl, showed a significantly higher retention of NP than that observed under saturated conditions and very similar experimental conditions. Water flow was simulated using the standard Richards equation. The hydrodynamic model parameters for unsaturated flow were estimated through independent drainage experiments. A new mathematical model was developed to describe TiO2 NP transport and retention on SWI and AWI. The model accounts for the variation of water content and water velocity as a function of depth and takes into account the presence of the AWI and its role as a NP collector. Comparisons with experimental data showed that the suggested modeled processes can be used to quantify the NPs retentions at the AWI and SWI. The suggested model can be used for both saturated and unsaturated conditions and for a rather large range of velocities.
通过在不同水饱和度和离子强度(IS)条件下的米级柱实验,研究了人造二氧化钛(TiO₂,金红石型)纳米颗粒(NP)在多孔介质中的传输。NP突破曲线表明,对于IS等于或小于3mM KCl的情况,TiO₂ NP在空气与水界面(AWI)以及固体与流体界面(SWI)上的保留不显著。对于较大的IS,保留情况取决于含水量和流体流速。在5mM KCl的IS条件下进行的实验表明,NP的保留率比在饱和条件和非常相似的实验条件下观察到的要高得多。使用标准理查兹方程对水流进行了模拟。通过独立的排水实验估算了非饱和流的水动力模型参数。开发了一个新的数学模型来描述TiO₂ NP在SWI和AWI上的传输和保留。该模型考虑了含水量和水流速度随深度的变化,并考虑了AWI的存在及其作为NP收集器的作用。与实验数据的比较表明,所建议的建模过程可用于量化NP在AWI和SWI处的保留率。所建议的模型可用于饱和和非饱和条件以及相当大的速度范围。