Abstract

The 300°C experiments were conducted in hermetic platinum ampoules with aqueous solution saturated by SiO2 with respect to quartz. The solute SiO2 concentration did not change with time in ampoules with the smooth walls, however in the ampoules with the induced roughness on their walls it decreased exponentially with time and amorphous silica precipitated on the ampoule walls contacted with the water vapor. The experimental results were explained by the distillation initiated through preferential water evaporation in the thin layer (<100 nm) at the meniscus edge and strengthened by the surface wall roughness because of the evaporation surface area increase at the wall wetting in the impregnation regime. This process was accompanied by the progressive disturbance of the equilibrium distribution of the dissolved silica between liquid water and vapor. The similar mechanism might exist in the systems of the different composition. It may initiate the continuous renewal of the water dissolving ability, which can lead at natural conditions to the migration of the voids partially filled by the solution.

Highlights

  • Water-rock interaction is studied using the quantitative data of thermodynamics, kinetics and dynamics based on the experimental and theoretical research of macrophenomena where the surface energy contribution is negligible

  • In the last time the geochemists became more attentive to the nanoparticles and nanofluids (

  • In the closed equilibrium system this property must be compensated by the preferable condensation over the bulk liquid surface, and it can lead to the distillation of aqueous solution

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Summary

Introduction

Water-rock interaction is studied using the quantitative data of thermodynamics, kinetics and dynamics based on the experimental and theoretical research of macrophenomena where the surface energy contribution is negligible. In the closed equilibrium system this property must be compensated by the preferable condensation over the bulk liquid surface, and it can lead to the distillation of aqueous solution. We proposed such mechanism for the explanation of the irreversible SiO2 transfer from the liquid water into the SiO2 solid phases situated in vapor [3,4]. The acceleration of the SiO2 transfer was found for the case of the rough textured wall.

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