Mechanism and kinetics of gypsum–anhydrite transformation in aqueous electrolyte solutions

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• 作者：Ghazal Azimi^a ; Vladimiros G. Papangelakis ; ^a ; ^{vladimiros.papangelakis@utoronto.ca"" rel=""nofollow}
• 关键词：Gypsum ; Anhydrite ; Hemihydrate ; Transformation kinetics ; Transformation mechanism ; Dissolution– ; precipitation
• 刊名：Hydrometallurgy
• 出版年：2011
• 出版时间：June 2011
• 年：2011
• 卷：108
• 期：1-2
• 页码：122-129
• 全文大小：1744 K

文摘

The transformation of gypsum into anhydrite at low temperatures under atmospheric pressure as well as at elevated temperatures (150 °C and 200 °C) inside an autoclave was investigated by monitoring changes in both the liquid and solid phases. The effect of temperature, sulfuric acid addition, anhydrite seeding and addition of sulfate and chloride salts on the transformation kinetics was determined. Anhydrite seeding, increasing temperature and acidity were found to accelerate the transformation process. Addition of NiSO₄ into sulfuric acid solutions hindered the transformation, whereas addition of NaCl resulted in acceleration. Based on the results obtained, gypsum–anhydrite transformation occurs through two different mechanisms at low and high temperatures, respectively. Below 100 °C, the mechanism consists of a direct dehydration step of gypsum to anhydrite (with no intermediate hemihydrate formation), resulting in the formation of anhydrite nuclei, followed by the growth of the nuclei through dissolution of gypsum and precipitation of stable anhydrite. Above 100 °C, however, the formation of intermediate hemihydrate was detected. Thus, the proposed mechanism under these conditions consists of step-wise dehydration of gypsum to hemihydrate and then to anhydrite, resulting in the formation of anhydrite nuclei, followed by the subsequent growth of the nuclei through dissolution–precipitation. Finally, the seeded transformation of gypsum into anhydrite was proposed as a practical tool for lowering the risk of CaSO₄ scale formation in hydrometallurgical processes.