Department of Soil Physics, Helmholtz Centre for Environmental Research-UFZ, Theodor-Lieser-Strasse 4, 06120 Halle-Saale, Germany.
Interdisciplinary Center for Scientific Computing, University of Heidelberg, Im Neuenheimer Feld 368, Raum 422, 69120 Heidelberg, Germany.
Sci Total Environ. 2015 Dec 1;535:113-21. doi: 10.1016/j.scitotenv.2015.03.023. Epub 2015 Mar 29.
Chemical factors and physical constraints lead to coupled effects during particle transport in unsaturated porous media. Studies on unsaturated transport as typical for soils are currently scarce. In unsaturated porous media, particle mobility is determined by the existence of an air-water interface in addition to a solid-water interface. To this end, we measured breakthrough curves and retention profiles of citrate-coated Ag nanoparticles in unsaturated sand at two pH values (5 and 9) and three different flow rates corresponding to different water contents with 1 mM KNO3 as background electrolyte. The classical DLVO theory suggests unfavorable deposition conditions at the air-water and solid-water interfaces. The breakthrough curves indicate modification in curve shapes and retardation of nanoparticles compared to inert solute. Retention profiles show sensitivity to flow rate and pH and this ranged from almost no retention for the highest flow rate at pH=9 to almost complete retention for the lowest flow rate at pH=5. Modeling of the breakthrough curves, thus, required coupling two parallel processes: a kinetically controlled attachment process far from equilibrium, responsible for the shape modification, and an equilibrium sorption, responsible for particle retardation. The non-equilibrium process and equilibrium sorption are suggested to relate to the solid-water and air-water interfaces, respectively. This is supported by the DLVO model extended for hydrophobic interactions which suggests reversible attachment, characterized by a secondary minimum (depth 3-5 kT) and a repulsive barrier at the air-water interface. In contrast, the solid-water interface is characterized by a significant repulsive barrier and the absence of a secondary minimum suggesting kinetically controlled and non-equilibrium interaction. This study provides new insights into particle transport in unsaturated porous media and offers a model concept representing the relevant processes.
化学因素和物理约束导致非饱和多孔介质中颗粒输运的耦合效应。目前,关于非饱和输运(典型的土壤特征)的研究还很少。在非饱和多孔介质中,颗粒迁移率除了固-水界面外,还取决于气-水界面的存在。为此,我们在两个 pH 值(5 和 9)和三个不同的流速下(对应于不同的含水量),用 1mM KNO3 作为背景电解质,测量了柠檬酸包覆的 Ag 纳米颗粒在非饱和砂中的穿透曲线和保留曲线。经典的 DLVO 理论表明,在气-水和固-水界面上存在不利的沉积条件。穿透曲线表明,与惰性溶质相比,纳米颗粒的形状发生了改变,出现了滞后。保留曲线对流速和 pH 值敏感,范围从 pH=9 时最高流速下几乎没有保留到 pH=5 时最低流速下几乎完全保留。因此,穿透曲线的建模需要耦合两个平行过程:远离平衡的动力学控制附着过程,负责形状改变,以及平衡吸附,负责颗粒滞后。非平衡过程和平衡吸附分别与固-水界面和气-水界面有关。这得到了扩展到疏水相互作用的 DLVO 模型的支持,该模型表明了可逆附着,其特征是在气-水界面处存在二次最小值(深度 3-5 kT)和排斥势垒。相比之下,固-水界面的特征是存在显著的排斥势垒和不存在二次最小值,这表明存在动力学控制和非平衡相互作用。这项研究为非饱和多孔介质中颗粒输运提供了新的见解,并提供了一个代表相关过程的模型概念。