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An alternative viewpoint is presented here, where the whole of diffraction space is occupied by scattering from many crystal planes, which when combined contribute to the peaks observed.
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Currently, (100), (110), and (111) crystal planes are widely studied in many kinds of processing experiments and computer numerical simulations [7, 10, 24, 25].
However, for many crystal growth faces this is not the case; faces which lack a mirror plane perpendicular to the lamella have vr≠vl, resulting in asymmetric curvature.
Instead, discharge of ions is favoured on crystal planes.
b Various crystal planes of ZnO Wurtzite structure.
Such crystal planes and orientation are not common for ZnO.
The main peaks and the corresponding crystal planes are identified.
Many research has shown that anatase TiO2 (101) is the most stable and frequently exposed surface of anatase oxide, and the diffusion of hydrogen atoms in anatase TiO2 (101) is much easier than in other crystal planes [31 33].
These peaks indicate that there are two CdO crystal planes parallel to the ZnO (0001) plane.
These independent slip planes belong to the {111} crystal planes family.
It has been reported that H ions absorption on the crystal planes could decrease the surface energies of the crystal planes and such absorption on different crystal planes can be affected by overpotential [3, 38].
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