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首页> 外文期刊>American Mineralogist >Structural relaxation around Cr3+ and the red-green color change in the spinel (sensu stricto)-magnesiochromite (MgAl2O4-MgCr2O4) and gahnite-zincochromite (ZnAl2O4-ZnCr2O4) solid-solution series
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Structural relaxation around Cr3+ and the red-green color change in the spinel (sensu stricto)-magnesiochromite (MgAl2O4-MgCr2O4) and gahnite-zincochromite (ZnAl2O4-ZnCr2O4) solid-solution series

机译:尖晶石(Sensu stricto)-镁铬铁矿(MgAl2O4-MgCr2O4)和针铁矿-锌铬铁矿(ZnAl2O4-ZnCr2O4)固溶体系列中Cr3 +周围的结构弛豫和红绿色变化

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摘要

Optical absorption spectra of flux-grown single crystals in the spinel s.s.-magnesiochromite and gahnite-zincochromite solid solutions were recorded with the aim of exploring variations in local Cr-O bond distance as a function of composition. With increasing Cr contents, the crystals vary in color from pale red to intensely red to dark greenish. These variations are reflected in the optical spectra by the position and intensity of the two spin-allowed electronic d-d transitions in six-coordinated Cr3+ at ~18000 (1) and 25000 cm–1 (2). From the shift of the 1 band position, a decrease in crystal field splitting, 10Dq, for six-coordinated Cr3+ with increasing Cr contents is evident in both solid-solution series. Based on published Cr-O bond distances for the CrO6 polyhedra in magnesiochromite and zincochromite of 1.995 and 1.991 Å, respectively, and applying the ligand field relationships, local Cr-O bond distances in gahnite and spinel with Cr contents at trace levels are determined to be 1.974(2) and 1.960(3) Å, respectively. These local Cr-O distances result in relaxation parameters () equal to 0.69(2) and 0.60(3) for Cr-O bonds in the Mg(Al1–xCrx)2O4 and Zn(Al1–xCrx)2O4 series, respectively. However, the presently obtained Racah B values indicate increasing Cr-O bond covalency with increasing Cr3+ contents. This suggests that color changes and accompanying 10Dq variations may be due to variations in Cr-O bond covalency along the two solid-solution series, without or with very minor local Cr-O bond distance variation. Consequently, the values obtained from the present optical absorption spectra should be regarded as minimum values.
机译:记录了 尖晶石ss-镁铬铁矿和针铁矿-锌铬铁矿固溶体 溶液中助熔剂生长的单晶的光吸收光谱,旨在探索变化Cr-O局部键距随组成的变化而变化。随着 Cr含量的增加,晶体的颜色从浅 红色到深红色到深绿色。这些变化在光谱中由六配位 Cr 反映在光谱中> 3 + 在〜18000( 1 )和25000 cm –1 2 )处。从 1 带位置的shift 开始,六配位Cr 3+ <的晶体场分裂 10Dq减小。在两个固溶体系列中,随着Cr含量的增加/ sup>是明显的。基于已发表的镁铬铁矿和 锌铬铁矿中CrO 6 多面体的Cr-O 键距,分别为1.995和1.991Å,以及应用配体场关系,测定痕量铬含量的针铁矿和尖晶石中的局部Cr-O键距离 分别为1.974(2)和1.960 (3)分别。这些局部 Cr-O距离导致Mg(Al )中Cr-O键的弛豫参数()等于0.69(2) 和0.60(3) 1–x Cr x 2 O 4 Zn(Al 1– x Cr x 2 O 4 系列。但是,目前 获得的Racah B值表明,随着Cr 3 + 含量的增加,Cr-O键的共价键 增加。这表明颜色变化 和伴随的10Dq变化可能是由于沿两个固溶系列的 Cr-O键共价变化而没有 或局部Cr-O键距离变化很小。因此, 从当前光吸收光谱获得的值 应被视为最小值。

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  • 来源
    《American Mineralogist》 |2010年第4期|456-462|共7页
  • 作者单位

    Department of Mineralogy, Swedish Museum of Natural History, SE-10405 Stockholm, Sweden;

    Dipartimento di Scienze della Terra, Sapienza Universitá di Roma, Piazzale Aldo Moro 5, I-00185 Roma, Italy;

    Department of Mineralogy, Swedish Museum of Natural History, SE-10405 Stockholm, Sweden;

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