NiO powders were synthesized using coprecipitation, sol‐gel, and hydrothermal synthesis methods. The powders were subjected to calcination in atmospheric air, followed by recalcination in an O2‐rich atmosphere at 800°C for 2 hours each. Characterization techniques such as scanning electron microscopy, X‐ray diffraction, energy dispersive X‐ray spectroscopy, and microRaman spectroscopy were utilized. The coprecipitation and hydrothermal methods resulted in disaggregated sub‐micrometric particles. The average size of particles obtained by coprecipitation method after calcination in atmospheric air and recalcination in O2‐rich atmosphere was 360 ± 140 nm and 400 ± 130 nm, respectively. Regarding the particles obtained by hydrothermal method, the average size was 190 ± 50 and 220 ± 80 nm for calcined in atmospheric air and recalcined in O2‐rich atmosphere, respectively. Conversely, the sol‐gel method produced particle aggregates with an average size of 430 ± 150 nm after calcination in atmospheric air and 500 ± 200 nm for calcination in O2‐rich atmosphere. X‐ray diffraction analysis revealed that only the hydrothermal method yielded pure NiO without additional Ni‐related phases, irrespective of the calcination procedure. In contrast, the coprecipitation sample exhibited a Ni2O3 phase after calcination in atmospheric air, which disappeared after recalcination in an O2‐rich atmosphere. The sol‐gel‐derived sample maintained a Ni phase after both calcination processes. Analysis of the crystallite size demonstrated an increase after recalcination in an O2‐rich atmosphere for the hydrothermal and sol‐gel derived samples, while a decrease was observed for the coprecipitation‐derived sample. Raman spectra exhibited defect‐enabled first‐order forbidden phonon modes that were sensitive to the synthesis route. The two magnon phonon modes also demonstrated dependency on the route, indicating variations in defect structures. Photocatalytic evaluation using methylene blue degradation in aqueous solutions indicated better performance for the powders recalcined in an O2‐rich atmosphere.This article is protected by copyright. All rights reserved