“…The preparation work-up and, specifically, the drying stage in air in the “wet” mechanochemical synthesis method, constitutes yet another oxygen source, possibly even more acute, since one deals at this stage with very reactive, high-surface-area nanopowders exposed to air for relatively long and variable periods of time. As a result, such oxidation by-products are detected for kesterite samples as metal sulfates including copper sulfate pentahydrate CuSO 2 •5H 2 O, zinc sulfate monohydrate ZnSO 4 •H 2 O, and, possibly, hydrated tin oxide SnO 2 •xH 2 O not only in the mechanochemical synthesis method [ 4 , 5 , 9 ] but also in other preparation routes [ 10 , 11 , 12 ]. It is instructive to note that in some kesterite studies, the presence of oxygen-bearing species is evident from inspection of the data, although it is not specifically acknowledged or appropriately commented on by authors [ 13 ] (e.g., XPS survey scans with the apparent O 1s band in the range of 529–531 eV for oxides or the S2p 3/2 /S2p 1/2 bands in the range of 167–172 eV for the sulfate group [SO 4 ] −2 ).…”