“…The observed peaks can be divided into three peaks O I , O II , and O III located at 530.2, 531.5, and 532.5 eV, respectively. The O I peak is assigned to In 2 O 3 lattice oxygen [22,23], while the O II peak is assigned to the oxygen ions in the oxygen vacancy regions [22,23]. For the O III peak, it can originate from the H 2 O absorbed on the surfaces of samples [23].…”