【摘要】 使用金刚石对顶砧高压装置(DAC)和同步辐射光源,对天然白钨矿进行了原位高压能量色散X射线衍射(EDXD)研究,实验最高压力为16.0GPa。在实验压力范围内观察到了一次白钨矿结构→钨锰铁矿结构的可逆相变:压力小于5.3GPa时为白钨矿结构(I41/a),在5.3～12.3GPa压力区间内为白钨矿结构与钨锰铁矿结构(P2/c)并存,大于12.3GPa时完全相变为钨锰铁矿结构。从键长、配位数和配位多面体角度对白钨矿→钨锰铁矿结构的相变机制进行了解释。更多还原

【Abstract】 In-situ high-pressure energy dispersive X-ray diffraction experiments on natural scheelite ( CaWO4) have been carried out at room temperature by using DAC device with a synchrotron radiation source at 4W2 High-Pressure Station of Beijing Synchrotron Radiation Facility. In pressures higher than 16. 0 GPa,a reversible phase transition from scheelite-structure to wolframite-structure was observed. With increasing pressure,CaWO4 kept the scheelite-structure until 5. 3 GPa,and then had a coexistence with scheelite-and wolframite-structures between 5. 3 GPa and 12. 3 GPa,and finally completely transformed to wolframite-structure at pressures above 12. 3 GPa. The mechanism of the phase transition from scheelite-to-wolframite was also explained in the views of bond length,coordinate number and coordinate polyhedron.更多还原