Abstract
Vibrational amplitudes in graphite are determined using the temperature dependent intensity diminution of the (002)-, (004)-, (110)- and (112)-reflections between room-temperature and 1900°C. Besides Lorentz polarization and atomic scattering factors the integrated intensities were corrected for thermal diffuse scattering (TDS). For this reason a modified Debye-model has been established to calculate the TDS in powder diagrams of layer structures.
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