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The obtained results help to clarify the relationship between the decomposition temperature and Hg occurrence.
X-ray diffraction and transmission electron microscopy reveal that some structural changes occur after cycling: there is an increase in particle size of the MgH2 phase, with separation between the magnesium and carbon phases, indicating a clear relationship between the decomposition temperature of MgH2 and its structure.
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The density and the spacing between the plates depend on the decomposition temperature and time.
However, the decomposition temperature is much higher than the PEMFC operating temperature.
Here, the decomposition temperature of SiCl4 is compatible with the Ni Si eutectic temperature (966 °C).
This temperature is 51.63 °C lower than the decomposition temperature of pure NaMgH3.
Tmax is the decomposition temperature corresponding to the maximum weight loss and relates to the maximum decomposition rate.
It is well known that variation of the cation species in the A and B sites influences the decomposition temperature of the jarosite structure and that other sulfate species also have highly variable decomposition temperatures.
Based on DSC and TGA results, the decomposition temperatures, the final decomposition mass, final decomposition temperature and enthalpy of process (ΔH d ) were evaluated.
The decomposition temperatures for those in sample no. 1 and sample no. 2 were 259 and 250 °C, respectively.
The increase in the difference between the thermal decomposition temperature and the melting point (ΔT∼100 °C) enabled the melt processing of PVA.
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