首页> 外文期刊>Physics and chemistry of minerals >The crystal and magnetic structure of Li-aegirine LiFe~(3+)Si_2O_6: a temperature-dependent study
【24h】

The crystal and magnetic structure of Li-aegirine LiFe~(3+)Si_2O_6: a temperature-dependent study

机译:锂铁LiFe〜(3+)Si_2O_6的晶体和磁性结构:与温度有关的研究

获取原文
获取原文并翻译 | 示例
       

摘要

Single crystals of Li-aegirine LiFe~(3+)Si_2O_6 were synthesized at 1573 K and 3 GPa, and a polycrystalline sample suitable for neutron diffraction was produced by ceramic sintering at 1223 K. LiFe~(3+)Si_2O_6 is monoclinic, space group C2/c, a = 9.6641(2) A, b = 8.6612(3) A, c = 5.2924(2) A, β = 110.12(1)°at 300 K as refined from powder neutron data. At 229 K Li-aegirine undergoes a phase transition from C2/c to P2_1/c. This is indicated by strong discontinuities in the temperature variation of the lattice parameters, especially for the monoclinic angle β and by the appearance of Bragg reflections (hkl) with h + k ≠ 2n. In the low-temperature form two non-equivalent Si-sites with = 1.622 A and = 1.624 A at 100 K are present. The bridging angles of the SiO_4 tetrahedra O3-O3-O3 are 192.55(8)°and 160.02(9)°at 100 K in the two independent tetrahedral chains in space group P2_1/c, whereas it is 180.83(9)°at 300 K in the high-temperature C2/c phase, i.e. the chains are nearly fully expanded. Upon the phase transition the Li-coordination changes from six to five. At 100 K four Li-O bond lengths lie within 2.072(4)-2.172(3) A, the fifth Li-O bond length is 2.356(4) A, whereas the Li-O3 A bond lengths amount to 2.796(4) A. From ~(57)Fe Mossbauer spectroscopic measurements between 80 and 500 K the structural phase transition is characterized by a small discontinuity of the quadrupole splitting. Temperature-dependent neutron powder diffraction experiments show first occurrence of magnetic reflections at 16.5 K in good agreement with the point of inflection in the temperature-dependent magnetization of LiFe~(3+)Si_2O_6. Distinct preordering phenomena can be observed up to 35 K. At the magnetic phase transition the unit cell parameters exhibit a pronounced magneto-striction of the lattice. Below T_N Li-aegirine shows a collinear antiferromagnetic structure. From our neutron powder diffraction experiments we extract a collinear antiferromagnetic spin arrangement within the a-c plane.
机译:在1573 K和3 GPa下合成了Li-aegirine LiFe〜(3+)Si_2O_6单晶,并通过在1223 K下进行陶瓷烧结制备了适合中子衍射的多晶样品。LiFe〜(3+)Si_2O_6是单斜晶空间C2 / c组,a = 9.6641(2)A,b = 8.6612(3)A,c = 5.2924(2)A,β= 110.12(1)°,在300 K下根据粉末中子数据精制而成。在229 K,锂亮氨酸经历了从C2 / c到P2_1 / c的相变。这由晶格参数的温度变化的强烈不连续性(特别是对于单斜角β)和h + k≠2n的布拉格反射(hkl)的出现来表明。在低温形式下,存在两个非等价的Si位,在100 K时 = 1.622 A和 = 1.624A。在空间群P2_1 / c中两个独立的四面体链中,SiO_4四面体O3-O3-O3的桥接角在100 K时为192.55(8)°和160.02(9)°,而在300 K时为180.83(9)°高温C2 / c相中的K,即链几乎完全膨胀。在相变之后,锂配位从六变为五。在100 K下,四个Li-O键长在2.072(4)-2.172(3)A内,第五个Li-O键长为2.356(4)A,而Li-O3 A键长为2.796(4) A.在80至500 K之间的〜(57)Fe Mossbauer光谱测量中,结构相变的特征在于四极分裂的不连续性很小。温度相关的中子粉末衍射实验表明,在16.5 K处首次出现磁反射,这与LiFe〜(3+)Si_2O_6的温度相关磁化的拐点非常吻合。可以观察到高达35 K的不同的预排序现象。在磁性相变时,晶胞参数显示出明显的晶格磁致伸缩。在T_N Li-aegirine下面显示了共线反铁磁结构。从我们的中子粉末衍射实验中,我们在a-c平面内提取了共线反铁磁自旋排列。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号