Transport of colloidal silica in unsaturated sand: Effect of charging properties of sand and silica particles. (July 2016)

• Record Type: Journal Article
• Authors: Fujita, Yosuke; Kobayashi, Motoyoshi
• Is Part Of: Chemosphere. Volume 154(2016)
• Page Start: 179
• Page End: 186
• Publication Date: 2016-07
• Subjects: Colloid transport -- Water contents -- Solution pH; Pollution -- Periodicals; Pollution -- Physiological effect -- Periodicals; Environmental sciences -- Periodicals; Atmospheric chemistry -- Periodicals; 551.511
• DOI: 10.1016/j.chemosphere.2016.03.105
• Languages: English
• ISSNs: 0045-6535

Abstract

Abstract: We have studied the transport of colloidal silica in various degrees of a water-saturated Toyoura sand column, because silica particles are widely used as catalyst carriers and abrasive agents, and their toxicity is reported recently. Since water-silica, water-sand, and air-water interfaces have pH-dependent negative charges, the magnitude of surface charge was controlled by changing the solution pH. The results show that, at high pH conditions (pH 7.4), the deposition of colloidal silica to the sand surface is interrupted and the silica concentration at the column outlet immediately reaches the input concentration in saturated conditions. In addition, the relative concentration of silica at the column outlet only slightly decreases to 0.9 with decreasing degrees of water saturation to 38%, because silica particles are trapped in straining regions in the soil pore and air-water interface. On the other hand, at pH 5 conditions (low pH), where sand and colloid have less charge, reduced repulsive forces result in colloidal silica attaching onto the sand in saturated conditions. The deposition amount of silica particles remarkably increases with decreasing degrees of water saturation to 37%, which is explained by more particles being retained in the sand column associated with the air-water interface. In conclusion, at higher pH, the mobility of silica particles is high, and the air-water interface is inactive for the deposition of silica. On the other hand, at low pH, the deposition amount increases with decreasing water saturation, and the particle transport is inhibited. Highlights: Transport of colloidal silica was examined in unsaturated sand column. Amount of silica deposition depends on solution pH even in unsaturated condition. Water contents were less effective on deposition amount at high pH condition. Water contents significantly affect deposition amount at low pH condition.