Department of Geology and Geophysics , University of Utah , Salt Lake City , Utah 84112 , United States.
Environ Sci Technol. 2019 Mar 5;53(5):2450-2459. doi: 10.1021/acs.est.8b06162. Epub 2019 Feb 22.
Recent experiments revealed that roughness decreases the gap in colloid attachment between favorable (repulsion absent) and unfavorable (repulsion present) conditions through a combination of hydrodynamic slip and surface interactions with asperities. Hydrodynamic slip was calibrated to experimentally observed tangential colloid velocities, demonstrating that slip length was equal to maximum asperity relief, thereby providing a functional relationship between slip and roughness metrics. Incorporation of the slip length in mechanistic particle trajectory simulations yielded the observed modest decrease in attachment over rough surfaces under favorable conditions, with the observed decreased attachment being due to reduced colloid delivery rather than decreased attraction. Cumulative interactions with multiple asperities acting within the zone of colloid-surface interaction were unable to produce the observed dramatic increased attachment and decreased reversibility with increased roughness under unfavorable conditions, necessitating inclusion of nanoscale attractive heterogeneity that was inferred to have codeveloped with roughness. Simulated attachment matched experimental observations when the spatial frequency of larger heterodomains (nanoscale zones of attraction) increased disproportionately relative to smaller heterodomains as roughness increased, whereas attachment was insensitive to asperity properties, including the number of interactions per asperity and asperity height; colloid detachment simulations were highly sensitive to these parameters. These cumulative findings reveal that hydrodynamic slip moderately decreases colloid bulk delivery, nanoscale heterogeneity dramatically enhances colloid attachment, and multiple interactions among asperities decrease detachment from rough surfaces.
最近的实验表明,粗糙度通过结合水动力滑移和与粗糙度的表面相互作用,降低了胶体在有利(无排斥)和不利(有排斥)条件下附着的间隙。水动力滑移根据实验观察到的切向胶体速度进行了校准,表明滑移长度等于最大粗糙度峰高,从而提供了滑移和粗糙度度量之间的功能关系。在机械粒子轨迹模拟中加入滑移长度,在有利条件下,在粗糙表面上观察到附着的适度减少,观察到的附着减少是由于胶体传递减少,而不是吸引力减少。在胶体-表面相互作用区域内的多个粗糙度作用的累积相互作用,无法在不利条件下产生观察到的附着显著增加和可逆性降低,需要包括推断与粗糙度共同发展的纳米级吸引力非均质性。当较大的异质域(纳米级吸引区)的空间频率相对于较小的异质域不成比例地增加时,模拟的附着与实验观察结果相匹配,而粗糙度增加时,附着对粗糙度特性(包括每个粗糙度的相互作用次数和粗糙度高度)不敏感;胶体脱离模拟对这些参数高度敏感。这些累积发现表明,水动力滑移适度降低胶体的整体输送,纳米级非均质性显著增强胶体的附着,并且粗糙度上多个相互作用降低了胶体的脱离。