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Low-temperature crystal structure evolution of (Na,Ca)(Cr,Mg)Si_2O_6 pyroxene

机译:(Na,Ca)(Cr,Mg)Si_2O_6辉石的低温晶体结构演变

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摘要

The crystal structure of a clinopyroxene with composition (Na_(0.75)Ca_(0.25))(Cr_(0.75)Mg_(0.25))Si_2O_6 was refined at 100, 150, 200, 250 and 298 K. The work was performed in the context of an investigation on the low-temperature behaviour of A~+M~(3+)Si_2O_6 (with A dominant in Na and M = transition elements) pyroxenes in order to provide new insights concerning the phase transition and anomalies recently found in the low-temperature behaviour of NaTiSi_2O_6 and NaGaSi_2O_6 compounds. The refinements were done in the C2/c space group (wR~2 between 0.048 and 0.068), and no change of symmetry was observed down to 100 K. Highly-anisotropic axial thermal expansion occurs with the scheme alpha_b >= alpha_a > alpha_c. The M2, M1 and T polyhedra expand with alpha_(M2) > alpha_(M1) > alpha_T, as generally observed in pyroxenes. A discontinuity in the Ml polyhedral volume is observed between 200 and 250 K, similar to the one observed in NaGaSi_2O_6 between 190 and 235 K. The atomic displacement parameters are scaled according to the following pattern: U_(M2) > U_(O2) > U_(O3) >= U_(O1) > U_T >= U_(M1). Comparison with previous data along the CaMgSi_2O-NaCrSi_2O_6 join suggests significant positional disorder for the 01 oxygen, due to repulsion of the 2p orbitals of O1 and the non-bonding 3d electrons of Cr.
机译:组成为(Na_(0.75)Ca_(0.25))(Cr_(0.75)Mg_(0.25))Si_2O_6的亚斜辉石的晶体结构分别在100、150、200、250和298 K下精炼。对A〜+ M〜(3+)Si_2O_6(A在Na中占主导地位,M =过渡元素)的辉石的低温行为的研究,以提供有关最近在低温中发现的相变和异常的新见解NaTiSi_2O_6和NaGaSi_2O_6化合物的高温行为。细化是在C2 / c空间组中完成的(wR〜2在0.048和0.068之间),直到100 K都没有观察到对称性变化。当方案为alpha_b> = alpha_a> alpha_c时,会发生高度各向异性的轴向热膨胀。如在辉石中通常观察到的,M2,M1和T多面体以alpha_(M2)> alpha_(M1)> alpha_T扩展。在200和250 K之间观察到M1多面体体积的不连续性,类似于在NaGaSi_2O_6中在190和235 K之间观察到的不连续性。原子位移参数根据以下模式进行缩放:U_(M2)> U_(O2)> U_(O3)> = U_(O1)> U_T> = U_(M1)。与沿CaMgSi_2O-NaCrSi_2O_6连接的先前数据进行的比较表明,由于O1的2p轨道的排斥和Cr的非键3d电子的排斥,01氧存在明显的位置混乱。

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