Department of Soil and Water Sciences, China Agricultural University, Beijing, 100193, China.
Department of Soil and Water Sciences, China Agricultural University, Beijing, 100193, China.
Water Res. 2020 Sep 15;183:116068. doi: 10.1016/j.watres.2020.116068. Epub 2020 Jun 20.
Saturated column experiments were conducted to systematically examine the influence of hydration on the detachment of nano- and micro-sized latex colloids (35 nm and 1 μm, respectively) from sand. The colloids were attached on the sand in primary minima (PM) using high ionic strength (IS) NaCl solutions. The PM were predicted to be shallower and located farther from sand surfaces with increasing IS due to the hydration force. Consequently, a greater amount of colloid detachment occurred in deionized water when the colloids were initially deposited at a higher IS. Atomic force microscopy (AFM) examinations showed that both nanoscale protruding asperities and large wedge-like valleys existed on the sand surface. The influence of these surface features on the interaction energies/forces was modeled by approximating the roughness as cosinoidal waves and two intersecting half planes, respectively. The PM were deep and attachment was irreversible at concave regions for all ISs, even if the hydration force was included. Conversely, colloids were weakly attached at protruding asperities due to a reduced PM depth, and thus were responsible for the detachment upon IS reduction. The AFM examinations confirmed that the adhesive forces were enhanced and reduced (or even completely eliminated) at concave and convex locations of sand surfaces, respectively. These results have important implications for surface cleaning and prediction of the transport and fate of hazardous colloids and colloid-associated contaminants in subsurface environments.
进行了饱和柱实验,以系统地研究水合作用对纳米和微米级乳胶胶体(分别为 35nm 和 1μm)从砂体上脱落的影响。胶体在初级最小势能(PM)中通过高离子强度(IS)NaCl 溶液附着在砂体上。由于水化力的作用,PM 预计会变浅,并且随着 IS 的增加而远离砂体表面。因此,当胶体最初在较高 IS 下沉积时,在去离子水中会发生更多的胶体脱落。原子力显微镜(AFM)检测表明,砂体表面存在纳米级的突出峰和大楔形谷。通过将粗糙度近似为余弦波和两个相交的半平面,分别对这些表面特征对相互作用能/力的影响进行了建模。在所有 IS 下,即使包括水化力,PM 也很深,并且在凹面区域的附着是不可逆的。相反,由于 PM 深度减小,胶体在突出的峰上附着较弱,因此在 IS 降低时会脱落。AFM 检测证实,在砂体表面的凹面和凸面位置,粘附力分别增强和减弱(甚至完全消除)。这些结果对于表面清洁以及预测危险胶体和胶体相关污染物在地下环境中的迁移和归宿具有重要意义。