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Kinetics and dynamics of mass-transfer-controlled mineral and bubble dissolution or growth: a review

机译:传质控制的矿物和气泡溶解或生长的动力学和动力学:综述

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In geology and daily life, kinetics and dynamics of particle (including crystal, droplet, and bubble) dissolution or growth in a liquid are a large class of often-encountered problems. The growth or dissolution of bubbles and drops are usually controlled by mass transfer, whereas the growth or dissolution of crystals may be controlled either by mass or heat transfer or by interface reaction. In this paper, recent advances in kinetics and dynamics of particle dissolution or growth controlled by mass transfer are reviewed, focusing on quantitative prediction models. Mass-transfer-controlled growth or dissolution can be further distinguished as diffusive (non-convective) or convective. For both types of particle dissolution or growth, approximate models are available for not only a single particle, but also multiple particles. These models have no free parameters. Hence, dissolution or growth rates can be calculated as long as the relevant physical and chemical properties are known, including: diffusivity in the liquid, viscosity of the liquid, and saturation condition between the particle and the liquid.
机译:在地质和日常生活中,颗粒(包括晶体,液滴和气泡)在液体中溶解或生长的动力学和动力学是一类经常遇到的问题。气泡和液滴的生长或溶解通常通​​过传质来控制,而晶体的生长或溶解则可以通过传质或传热或通过界面反应来控制。在本文中,综述了受质量转移控制的颗粒溶解或生长的动力学和动力学方面的最新进展,重点是定量预测模型。传质控制的生长或溶解可进一步区分为扩散性(非对流性)或对流性。对于两种类型的粒子溶解或增长,近似模型不仅适用于单个粒子,而且适用于多个粒子。这些模型没有自由参数。因此,只要已知相关的物理和化学性质,就可以计算出溶解或生长速率,包括:液体中的扩散率,液体的粘度以及颗粒与液体之间的饱和条件。

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