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模拟微粉方解石溶解对淡化水的再矿化作用。

Modeling Remineralization of Desalinated Water by Micronized Calcite Dissolution.

机构信息

Rabin Desalination Laboratory, Technion-Israel Institute of Technology , Haifa 32000, Israel.

出版信息

Environ Sci Technol. 2017 Nov 7;51(21):12481-12488. doi: 10.1021/acs.est.7b03069. Epub 2017 Oct 30.

Abstract

A widely used process for remineralization of desalinated water consists of dissolution of calcite particles by flow of acidified desalinated water through a bed packed with millimeter-size calcite particles. An alternative process consists of calcite dissolution by slurry flow of micron-size calcite particles with acidified desalinated water. The objective of this investigation is to provide theoretical models enabling design of remineralization by calcite slurry dissolution with carbonic and sulfuric acids. Extensive experimental results are presented displaying the effects of acid concentration, slurry feed concentration, and dissolution contact time. The experimental data are shown to be in agreement within less than 10% with theoretical predictions based on the simplifying assumption that the slurry consists of uniform particles represented by the surface mean diameter of the powder. Agreement between theory and experiment is improved by 1-8% by taking into account the powder size distribution. Apart from the practical value of this work in providing a hitherto lacking design tool for a novel technology. The paper has the merit of being among the very few publications providing experimental confirmation to the theory describing reaction kinetics in a segregated flow system.

摘要

一种广泛使用的淡化水再矿化方法包括通过酸化的淡化水流经填充有毫米大小的方解石颗粒的床层,使方解石颗粒溶解。另一种方法是通过酸化的淡化水与微米大小的方解石颗粒的浆液流使方解石溶解。本研究的目的是提供理论模型,以设计通过碳酸钙浆液溶解与碳酸和硫酸的再矿化过程。本文提供了大量的实验结果,展示了酸浓度、浆液进料浓度和溶解接触时间的影响。实验数据与基于简化假设的理论预测值之间的偏差小于 10%,该简化假设认为浆液由通过粉末的表面平均直径表示的均匀颗粒组成。通过考虑粉末尺寸分布,理论预测值与实验值的偏差提高了 1-8%。除了为一种新的技术提供了一个迄今为止缺乏的设计工具,这一工作具有实际价值之外,本文的优点还在于它是少数几篇提供了对描述分隔流系统反应动力学的理论进行实验验证的出版物之一。

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