Kinetics of uranium extraction from coffinite—A comparison with other common uranium minerals

铀矿 溶解 萃取(化学) 化学 铀矿石 矿物学 矿物 核化学 环境化学 冶金 材料科学 色谱法 有机化学 物理化学
作者
Hailey S Reynolds,Rahul Ram,Mark I. Pownceby,Yi Yang,Miao Chen,James Tardio,Lathe A. Jones,Suresh K. Bhargava
出处
期刊:Transactions of Nonferrous Metals Society of China [Elsevier BV]
卷期号:28 (10): 2135-2142 被引量:6
标识
DOI:10.1016/s1003-6326(18)64858-7
摘要

A synthetic coffinite was hydrothermally prepared and characterized before conducting a series of acid sulfate leach tests under conditions of relevance to uranium extraction. The results were then compared with similar studies on synthetic versions of the related U4+ minerals uraninite (UO2) and brannerite (UTi2O6) to identify and differentiate the rate and U extraction among these important uranium minerals. Tests examining the influence of residence time on uranium dissolution from synthetic coffinite, uraninite and brannerite showed that under similar experimental conditions, complete dissolution of uranium from coffinite was obtained between 36 and 48 h. The activation energy for this reaction was calculated to be 38.4 kJ/mol. This represented a significantly slower rate of dissolution than that indicated for uraninite which dissolved in 3 h (Ea=15.2 kJ/mol). The synthetic brannerite was leached at a much slower rate than the coffinite and reached a maximum dissolution of ∼18% U in 144 h (Ea=42–84 kJ/mol). The clear differentiation in rates and U extraction among the three minerals is consistent with previous literatures which suggest that in terms of leachability, uraninite>coffinite>brannerite. It is expected that the presence of impurities in natural coffinites would further inhibit leachability.

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