Abstract

Colloid transport experiments focusing on the initial deposition stage in water-unsaturated sand columns were conducted. To examine the effect of electrostatic interaction in the unsaturated condition, negatively and positively charged silica colloids were used for column transport experiments under different salt concentrations. The results of the column experiments were analyzed based on the colloid filtration theory and the deposition rate constants, and the single collector efficiency was calculated. The deposition rate constants of both negatively and positively charged silica in a water-unsaturated condition are larger than those in a water-saturated condition at an equivalent salt concentration, because the interface between air and water acts as an additional deposition site. The negatively charged silica shows the salt concentration, above which electric double layer (EDL) repulsion can be neglected, and the salt concentration is called critical deposition concentration (CDC). The CDCs were almost the same values in water-saturated as well as unsaturated conditions. The deposition rate constants of the positively charged silica were slightly increased at 0.05 mM due to the EDL attractive forces in the saturated condition. However, we could not see the significant effects of the EDL attractive force in the unsaturated condition in this study. Also, the present results demonstrated that a correlation equation for calculating collector efficiency can be applied to the non-spherical collector particles.

Highlights

  • It has been very important to understand the transport phenomena of colloidal particles in porous media for controlling deep-bed filtration and predicting contaminants’ fates in aquifers [1,2]

  • While we cannot discriminate between the effects of each deposition mechanism, we find that the total deposition rate in the water-unsaturated the effects of each deposition mechanism, we find that the total deposition rate in the watercondition has a critical deposition concentration similar to that of the water-saturated condition

  • We performed colloid transport experiments in packed beds of sand particles focusing on the initial deposition stage in water-saturated and unsaturated conditions

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Summary

Introduction

It has been very important to understand the transport phenomena of colloidal particles in porous media for controlling deep-bed filtration and predicting contaminants’ fates in aquifers [1,2]. Colloidal particles stimulate the contaminants’ transport, or the colloidal particles themselves act as harmful contaminants in the soil [3,4,5]. More and more researches have been performed to clarify the effect of solution chemistry, the surface properties of particles, flow rate, colloid size, and water content on colloid transport [6,7,8,9,10,11,12]. Silica and surface-modified silica particles are often utilized as industrial materials—such as abrasive agents, carriers of catalysts, and composite materials. Radioactive spherical particles of silicate glass released by the accident of Fukushima Daiichi Nuclear

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