Abstract H 2 evolution and O 2 reduction have been investigated (by means of a solar simulator) for α‐Fe2O3 powders and colloids as a function of electrolyte pH.
Syafikah Huda Paiman, Mukhlis A. Rahman, Tetsuo Uchikoshi, Nik Abdul Hadi Md Nordin, Nur Hashimah Alias, Norfadhituladha Abdullah, Khairul Hamimah Abas, Mohd Hafiz Dzarfan Othman, Juhana Jaafar, Ahmad Fauzi Ismail
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