, which are the main components of atmospheric particles, were investigated using in situ diffuse reflectance infrared Fourier transform spectroscopy (in situ DRIFTS), ion chromatography (IC), temperature-programmed desorption (TPD), X-ray diffraction (XRD) and Brunauer-Emmett-Teller (BET) methods. The main products and intermediates of the heterogeneous oxidation of OCS on these oxides were identified with in situ DRIFTS and IC. The reaction mechanism and kinetics were also discussed. It is found that the reaction mechanism on these mineral oxides is the same as that on Al 2 O 3 for the same final products and the intermediates at room temperature. Namely, OCS can be catalytically oxidized to produce surface SO 4 2− species and gaseous CO 2 through the surface hydrogen thiocarbonate (HSCO 2 carbonyl sulfide, mineral oxides, sulfate, heterogeneous reaction, in situ DRIFTS Carbonyl sulfide (OCS) is one of the most abundant sulfur containing species in the atmosphere. It is relatively inert in the troposphere [1,2] and can be transported into stratosphere, where its photolysis is the important source of stratospheric sulfate aerosol [1][2][3][4]