Zheng, Jiayi, Weng, Changzhou, Tian, Chen, Zhang, Wenchao, Qin, Jiemin, Li, Xiaoqin, Liu, Weizhen, Zhang, Jing, and Lin, Zhang
• Efficient two-step phase transition extracted valuable metals from gypsum. • Path-0.5 outpaced path-0, achieving 99.9 % Cr and 98.8 % Cd extraction. • Atom rearrangement in two-step transition triggered atom remove form the lattice. • Extraction efficiencies for trace Pb, Zn, Hg, and As were > 98.5 %, and 95.6 % for Sr. Retrieving valuable metals (VMs) from industrial waste is an attractive approach to reduce the continuous consumption of metallic resources and prevent the environmental contamination by heavy metals. However, metal extraction efficiencies are extremely low due to their entrapment in crystal lattices. Herein, a universal strategy for extracting VMs from gypsum (CaSO 4 ·2H 2 O), a common industrial waste, was reported using a two-step phase transition of dehydration–rehydration; metal extraction was achieved by designing an appropriate phase transition route and controlling the phase transformation kinetics. As the phase transition route to CaSO 4 ·0.5H 2 O (path-0.5) proceeded faster than that to CaSO 4 (path-0), higher extraction efficiencies were realized for Cr (99.9%) and Cd (98.8%) from gypsum. Mechanistic investigations indicated that during the selected path-0.5 dehydration, water molecule loss from gypsum initiated a direct solid-state transformation, triggering the first rearrangement of local atoms and excluding partially incorporated metals from the CaSO 4 ·0.5H 2 O lattice. The subsequent rehydration from CaSO 4 ·0.5H 2 O to CaSO 4 ·2H 2 O, with a phase transition rate faster than that of path-0, triggered the secondary atom rearrangement. The synergism between the two atomic rearrangements finally led to the complete release of trapped metals. Additionally, this strategy was used for retrieving other metals (e.g., Pb, Zn, Hg, As, and Sr) from gypsum, thereby potentially offering a new approach for designing an appropriate phase transition route for extracting VMs from other hydrous minerals. [ABSTRACT FROM AUTHOR]