球霰石
方解石
无水的
奥斯特瓦尔德成熟
化学工程
碳酸钙
水溶液
文石
过饱和度
材料科学
化学
矿物学
纳米技术
有机化学
工程类
作者
Yang Ding,Yunyi Liu,Junyou Yang,Hongxu Yan,Ming Wang,Dan Wang,Xiaoying Lü,Bin Wang,Tianbo Fan,Hongfan Guo
标识
DOI:10.1016/j.powtec.2018.04.056
摘要
Polymorphism- or morphology-controllable synthesis of CaCO3 is of significance. Usually only calcite CaCO3 can be obtained from the ordinary CO2-Ca(OH)2 solution route; the very low solubility of Ca(OH)2 also causes many defects with this route. The route by CaCl2 and Na2CO3 exhibits some advantages, but the consumption of Na2CO3 is a deficiency. Therefore, this work studies the precipitation of CaCO3 with CaCl2 in NH3-CO2 aqueous solution, which will make the overall reaction “CaCO3 → CaCO3” if tracing the origin of the reactants. A main focus of the present work is to elucidate how to obtain various CaCO3 polymorphs with different morphologies through this synthesis system and the corresponding crystal growth mechanism. The results show that, just by simply regulating the reaction conditions, all three anhydrous CaCO3 polymorphs with various morphologies (e.g., cubic, lamellar, spherical, needle-like and branched) can be obtained in the absence of any additives. The crystal growth process can be well explained based on either Ostwald ripening or dissolution-recrystallization mechanism, depending on the reaction conditions. In addition, the rare phase transition of metastable vaterite to metastable aragonite can also be obtained from the present synthesis system, besides the usual phase transition of vaterite to the most thermodynamically stable calcite. This work provides the essential theoretical support for further developing a green process for CaCO3 production by using various calcium-containing carbonate minerals, such as limestone, calcite and dolomite.
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