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A Cr3+ luminescence study of spodumene at high pressures: Effects of site geometry, a phase transition, and a level-crossing

机译:高压下锂辉石的Cr3 +发光研究:位点几何形状,相变和平交的影响

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摘要

Cr3+ luminescence of the green Cr-bearing variety of spodumene (LiAlSi2O6) has been studied under hydrostatic conditions up to similar to 15 GPa. R-line luminescence is a particularly sensitive site-specific probe of the Al-site, and high-pressure phase transitions that affect the symmetry or electron density at this site should produce obvious changes in the luminescence spectra. Thus, the nature of Cr3+ luminescence is probed across known and possible phase transitions in spodumene. Discontinuous shifts of the R-lines and their sidebands to higher energy at 3.2 GPa are associated with the C2/c to P2(1)/c phase transition. Both R-lines and sidebands shift to lower energy after the 3.2 GPa transition up to similar to 15 GPa. The C2/c to P2(1)/c phase transition is confirmed to be first order in nature based on its observed hysteresis on decompression, and R-line and sideband measurements give no evidence of a second proposed transition up to similar to 15 GPa. The splitting between the R-1 and R-2 bands is dramatically enhanced by pressure, with the split decreasing at the phase transition. These trends correspond to pressure-induced shifts in the distortion of the M1 site, and a likely shift in off-centeredness of the Cr3+ ion. Pressure-induced decreases in line widths are consistent with the R-lines shifting at slower rates than the phonons to which they are most closely coupled, as demonstrated by large pressure shifts of vibronic peaks. Observations of a pressure-induced cross-over between the T-4(2) and E-2 levels of the Cr3+ ion indicate that spodumene undergoes a shift from an intermediate strength crystal field environment to a high strength crystal field environment at pressures between ambient and 3.2 GPa.
机译:已经研究了在高达15 GPa的静水压力条件下研究了绿色辉石形锂辉石(LiAlSi2O6)的Cr3 +发光。 R线发光是对Al站点特别敏感的特定站点探针,影响该站点对称性或电子密度的高压相变应会在发光光谱中产生明显的变化。因此,在锂辉石中已知和可能的相变中探究了Cr3 +发光的性质。 R线及其边带在3.2 GPa处向更高能量的不连续位移与C2 / c到P2(1)/ c的相变有关。在3.2 GPa过渡到接近15 GPa之后,R线和边带都转移到较低的能量。基于C2 / c到P2(1)/ c的相变,基于其在减压时观察到的滞后现象,其性质被确认为一阶,并且R线和边带测量没有证据表明第二种拟议的相变达到15 GPa 。 R-1和R-2谱带之间的分离因压力而显着增强,在相变处该分离减小。这些趋势对应于压力引起的M1位置变形的偏移,以及Cr3 +离子偏心的偏移。压力引起的线宽减小与R线的移动速度比其最紧密耦合的声子慢,这与振动峰的大压力移动所证明的一致。压力诱导的Cr3 +离子的T-4(2)和E-2水平之间的交叉观察表明,锂辉石在环境压力与环境压力之间从中等强度晶体场环境转变为高强度晶体场环境和3.2 GPa。

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