The iron ores of the Gushan mine occur in the contact zone of a Mesozoic dioriteintrusion and are composed primarily of hematite microcrystallites and chalcedony. Thehematite microcrystallites have undergone post-mine...The iron ores of the Gushan mine occur in the contact zone of a Mesozoic dioriteintrusion and are composed primarily of hematite microcrystallites and chalcedony. Thehematite microcrystallites have undergone post-mineralization recrystallization and coarseningwith resultant formation of lath-shaped hematite porphyroblasts. Microscopic investigation reveals that recrystallization and coarsening of the hematite ores of the Gushan mine took placewithout the formation of new nuclei, due to the coalescence of the microcrystallites. The wholeprocess could have begun with the mutual approach of the microcrystallites, followed by grainrotation to realize parallelism and ending by the welding of these grains to form optically homogeneous porphyroblastic hematite.展开更多
The dehydrating activation energies of the hematite with several doped ions used for the alcohol sensor were determinated by thermogravimetric differential thermal analyzer (TG DTA) and the grain size of the samples w...The dehydrating activation energies of the hematite with several doped ions used for the alcohol sensor were determinated by thermogravimetric differential thermal analyzer (TG DTA) and the grain size of the samples were observed with TEM. The hematites with different doping amounts of Sn 4+ were investigated by Mssbauer spectrometer. It shows that the different doped ion is of influence for grain growth of the hematite. The decrease of grain size stemmed from the doped ion causes gas sensitivity for alcohol to increase and the dehydrating activation energy to decrease correspondingly. When the different amounts of Sn 4+ is doped in hematite, the microstructure of the hematite can be influenced.展开更多
文摘The iron ores of the Gushan mine occur in the contact zone of a Mesozoic dioriteintrusion and are composed primarily of hematite microcrystallites and chalcedony. Thehematite microcrystallites have undergone post-mineralization recrystallization and coarseningwith resultant formation of lath-shaped hematite porphyroblasts. Microscopic investigation reveals that recrystallization and coarsening of the hematite ores of the Gushan mine took placewithout the formation of new nuclei, due to the coalescence of the microcrystallites. The wholeprocess could have begun with the mutual approach of the microcrystallites, followed by grainrotation to realize parallelism and ending by the welding of these grains to form optically homogeneous porphyroblastic hematite.
文摘The dehydrating activation energies of the hematite with several doped ions used for the alcohol sensor were determinated by thermogravimetric differential thermal analyzer (TG DTA) and the grain size of the samples were observed with TEM. The hematites with different doping amounts of Sn 4+ were investigated by Mssbauer spectrometer. It shows that the different doped ion is of influence for grain growth of the hematite. The decrease of grain size stemmed from the doped ion causes gas sensitivity for alcohol to increase and the dehydrating activation energy to decrease correspondingly. When the different amounts of Sn 4+ is doped in hematite, the microstructure of the hematite can be influenced.