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Optical spectroscopic study of tetrahedrally coordinated Co2+ in natural spinel and staurolite at different temperatures and pressures

机译:在不同温度和压力下天然尖晶石和十字沸石中四面体配位的Co2 +的光谱研究

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摘要

Optical absorption spectra of natural Co-bearing spinel and staurolite were studied at different tem-peratures and pressures. In both minerals, two broad, intense structured bands in the range 5500–8000 and 15 000–19 000 cm–1, caused by electronic spin-allowed transitions 4A2 → 4T1(4F) and 4A2 → 4T1(4P) of IVCo2+ are the predominant absorption features. In addition, in both cases broad bands, derived from spin-allowed electronic transitions 4E → 4T2 of IVFe2+, appear in the near infrared range partly overlapping the bands caused by IVCo2+. In staurolite the NIR range of the spectra are complicated by intense sharp lines of OH-vibrations at around 3400 cm–1. In spinel, with a regular tetrahedral site, the splitting of the spin-allowed bands I and II of IVCo2+ is assumed to be caused by spin-orbit and vibronic coupling. In staurolite, the splitting is stronger due to the additional low-symmetry crystal field effect of IVCo2+. It is found that the effect of temperature and pressure on the behavior of the 4A2 → 4T1(4P) bands of IVCo2+ in the two minerals are rather similar, in contrast to our findings for the spin-allowed bands of IVFe2+ in spinel and staurolite. This is interpreted as a manifestation of a dynamic Jahn-Teller effect for IVFe2+ and lack of it in case of IVCo2+.
机译:研究了天然含钴尖晶石和十字沸石在不同温度和压力下的光吸收光谱。在这两种矿物中,IVCo2 +的电子自旋允许跃迁4A2→4T1(4F)和4A2→4T1(4P)引起了在5500–8000和15,000–19 000 cm-1范围内的两个宽的,强烈的结构化带。主要吸收特征。此外,在两种情况下,源自IVFe2 +的自旋允许电子跃迁4E→4T2的宽频带都出现在近红外范围内,与IVCo2 +引起的频带部分重叠。在星形陨石中,光谱的近红外范围由于在3400 cm-1附近的强烈的OH振动尖锐线而变得复杂。在具有规则四面体位点的尖晶石中,IVCo2 +的自旋允许带I和II的分裂被认为是由自旋轨道和振动耦合引起的。在星形石中,由于IVCo2 +的附加低对称性晶体场效应,分裂更强。我们发现,温度和压力对两种矿物中IVCo2 +的4A2→4T1(4P)谱带行为的影响非常相似,这与我们在尖晶石和星形石中IVFe2 +的自旋允许谱带的发现相反。这被解释为IVFe2 +的动态Jahn-Teller效应的表现,而在IVCo2 +的情况下则缺乏动态。

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