Litcius/Paper detail

In Situ Synchrotron X‐ray Diffraction Studies of the Mechanochemical Synthesis of ZnS from its Elements

Hilke Petersen, Steffen Reichle, Sebastian Leiting, Pit Losch, Wolfgang Kersten, Tobias Rathmann, Jochi Tseng, Martin Etter, Wolfgang Schmidt, Claudia Weidenthaler

2021Chemistry - A European Journal26 citationsDOIOpen Access PDF

Abstract

Abstract Mechanochemistry, as a synthesis tool for inorganic materials, became an ever‐growing field in material chemistry. The direct energy transfer by collision of the educts with the milling media gives the possibility to design environmental‐friendly reactions. Nevertheless, the underlying process of energy transfer and hence the kinetics of mechanosynthesis remain unclear. Herein, we present in situ synchrotron X‐ray diffraction studies coupled with pressure measurements performed during the formation of ZnS and the subsequent phase transition (PT) from the hexagonal to the cubic modification. Milling Zn and S 8 results in the sublimation of S 8 , observed by a sudden pressure increase. Simultaneously, the hexagonal metastable ZnS‐modification (wurtzite) forms. Via detection of the pressure maximum, the exact start of the wurtzite formation can be determined. Immediately after the formation of wurtzite, the structural PT to the thermodynamic stable cubic modification sphalerite takes place. This PT can be described by the Prout‐Tompkins equation for autocatalytic reactions, similar to thermally induced PT in sulfur vapor at high temperatures (T>1133 K). The increase in the reactivity of the wurtzite formation is explained by the reaction in sulfur vapor and the induction of defect structures by the collisions with the milling media.

Topics & Concepts

Wurtzite crystal structureMechanosynthesisMechanochemistrySphaleriteCrystallographyChemistrySynchrotronMaterials scienceChemical engineeringChemical physicsNanotechnologyHexagonal crystal systemMineralogyBall millMetallurgyOpticsEngineeringPhysicsPyriteThermal and Kinetic AnalysisCrystallography and molecular interactionsHigh-pressure geophysics and materials