Nazir Muhammad Kashif, Dyer Laurence, Tadesse Bogale, Albijanic Boris, Kashif Nadia
Western Australia School of Mines, Curtin University, Kalgoorlie, WA, 6430, Australia.
Heliyon. 2023 Feb 13;9(3):e13712. doi: 10.1016/j.heliyon.2023.e13712. eCollection 2023 Mar.
Calcination of spodumene is a pre-treatment stage in preparation for sulfation roasting and leaching in lithium recovery. During calcination, α-spodumene (less reactive, monoclinic crystal structure) is converted to β-spodumene (more reactive, tetragonal crystal structure). A third, metastable γ-phase has been identified at lower temperatures than full conversion to the β-phase. It has been previously observed that calcination greatly alters the physical properties of the various minerals in pegmatite ores, impacting comminution energy and liberation. Thus, this work investigates the relationships between calcination temperatures and the physical behaviour of hard rock lithium ores. The results showed that the increase in calcination temperature resulted in a higher lithium deportment in the finest size fraction (-0.6 mm) and thus a higher lithium grade and recovery. The samples calcined at 813.15 K and 1223.15 K did not show a significant increase in lithium grades in the finest size fraction. This work shows the incremental change in the physical properties of various minerals in the ore with increasing calcination temperature.
锂辉石的煅烧是锂回收过程中进行硫酸化焙烧和浸出的预处理阶段。在煅烧过程中,α-锂辉石(活性较低,单斜晶体结构)会转变为β-锂辉石(活性较高,四方晶体结构)。在低于完全转变为β相的温度下,已鉴定出第三种亚稳γ相。此前已观察到,煅烧会极大地改变伟晶岩矿石中各种矿物的物理性质,影响粉碎能量和矿物解离。因此,本研究调查了煅烧温度与硬岩锂矿石物理行为之间的关系。结果表明,煅烧温度的升高导致最细粒度级分(-0.6毫米)中的锂分布更高,从而锂品位和回收率也更高。在813.15K和1223.15K下煅烧的样品在最细粒度级分中的锂品位没有显著增加。这项工作表明,随着煅烧温度的升高,矿石中各种矿物的物理性质会发生渐进变化。