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Numerical Simulation of the Polycondensation of Orthosilicic Acid and of the Formation of Silica Particles in Hydrothermal Solutions

机译:替代硅酸缩聚的数值模拟及水热溶液中二氧化硅颗粒的形成

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摘要

This paper reports numerical modeling work for the polycondensation of orthosilicic acid (OSA) and the growth of the number of silica particles (SiO2) in hydrothermal solutions under a variety of physical and chemical conditions: temperature, pH, ionic strength, etc. We have derived relationships to calculate the concentration of orthosilicic acid and the mean radii of silica particles in relation to time and made plots showing the distribution of particles over size. The results were compared with experimental data. This study is important for investigating the role of colloidal silica in hydrothermal mineralization and for practical extraction and applications of silica, as well as for synthesis of minerals.
机译:本文报告了在各种物理和化学条件下的硅酸(OSA)的缩聚和水热溶液中二氧化硅颗粒(SiO 2)的生长的数值模拟工作:温度,pH,离子强度等。我们 衍生的关系,以计算与时间和制造颗粒分布尺寸的时间和制造图中硅酸的浓度和二氧化硅颗粒的平均半径。 将结果与实验数据进行比较。 该研究对于研究胶体二氧化硅在水热矿化中的作用以及二氧化硅的实际提取和应用,以及合成矿物质的作用非常重要。

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    Russian Acad Sci Far East Branch Geotechnol Res Ctr Severo Vostochnoe Shosse 30 A-Ya 56 Petropavlovsk Kamchatski 683002 Russia;

    Moscow MV Lomonosov State Univ Dept Chem Moscow 119991 Russia;

    Vitus Bering Univ Kamchatka Ul Leningradskaya 4 Petropavlovsk Kamchatski 683032 Russia;

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  • 正文语种 eng
  • 中图分类 地球物理学;
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