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Dapeng Cao

Researcher at Nanjing University

Publications -  13
Citations -  683

Dapeng Cao is an academic researcher from Nanjing University. The author has contributed to research in topics: Photocurrent & Water splitting. The author has an hindex of 8, co-authored 13 publications receiving 621 citations. Previous affiliations of Dapeng Cao include Nanjing University of Posts and Telecommunications.

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Cathodic shift of onset potential for water oxidation on a Ti4+ doped Fe2O3 photoanode by suppressing the back reaction

TL;DR: In this paper, a surface corrosion method was proposed to shift the photocurrent onset potential cathodically for water oxidation on a Ti4+ doped Fe2O3 by about 100 mV.
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A co-catalyst-loaded Ta(3)N(5) photoanode with a high solar photocurrent for water splitting upon facile removal of the surface layer.

TL;DR: Surface exfoliation: A Ta3 N5 photoanode prepared by a thermal oxidation and nitridation method shows a high solar photocurrent, which is currently the highest achieved by a Ta 3 N5photoanode.
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Chiral and Porous Coordination Polymers Based on an N-Centered Triangular Rigid Ligand

TL;DR: In this paper, four cadmium and cobalt coordination polymers with unique structures and topologies have been successfully synthesized under solvothermal conditions by employing an elongated triangular rigid N-containing ligand tris(4-(1H-imidazol-1-yl)phenyl)amine (TIPA) and 5-hydroxyisophthalic acid (5-OH-H2bdc) as anion coligand.
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Recent progress in photoelectrochemical water splitting for solar hydrogen production

TL;DR: In this article, several new strategies to enhance the performance of a water splitting photoelectrochemical (PEC) cell, such as surface exfoliation, suppressing back reaction and loading dual-layer catalysts, are discussed.
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A transparent Ti4+ doped hematite photoanode protectively grown by a facile hydrothermal method

TL;DR: In this paper, the thickness of pure Fe2O3 films increases initially and then decreases, while thickness of the Ti4+ doped samples always increases and reaches plateau values when the hydrothermal time is prolonged.