...
首页> 外文期刊>International Journal of Quantum Chemistry >Magnetic ordering and spin structure in Ca-bearing clinopyroxenes CaM2+(Si, Ge)2O6, M=Fe, Ni, Co, Mn
【24h】

Magnetic ordering and spin structure in Ca-bearing clinopyroxenes CaM2+(Si, Ge)2O6, M=Fe, Ni, Co, Mn

机译:含Ca的亚斜基芴CaM2 +(Si,Ge)2O6,M = Fe,Ni,Co,Mn的磁有序和自旋结构

获取原文
获取原文并翻译 | 示例
           

摘要

The compounds CaFeSi2O6 (hedenbergite), CaNiGe2O6, CaCoGe2O6 and CaMnGe2O6 have been synthesized by hydrothermal or ceramic sintering techniques and were subsequently characterized by SQUID magnetometry and powder neutron diffraction in order to determine the magnetic properties and the spin structure at low temperature. All four compounds reveal the well-known clinopyroxene structure-type with monoclinic symmetry, space group C2/c, Z=4 at all temperatures investigated. Below 35 K hedenbergite shows a ferromagnetic (FM) coupling of spins within the infinite M1 chains of edge-sharing octahedra. This FM coupling dominates an antiferromagnetic (AFM) coupling between neighbouring chains. The magnetic moments lie within the a–c plane and form an angle of 43° with the crystallographic a-axis. Magnetic ordering in CaFeSi2O6 causes significant discontinuities in lattice parameters, Fe–O bond lengths and interatomic Fe–Fe distances through the magnetic phase transition, which could be detected from the Rietveld refinements of powder neutron diffraction data. CaCoGe2O6 and CaNiGe2O6 show magnetic ordering below 18 K, the spin structures are similar to the one in hedenbergite with an FM coupling within and an AFM coupling of spins between the M1 chains. The moments lie within the a–c plane. The paramagnetic Curie temperature, however, decreases from CaFeSi2O6 (+40.2 K) to CaCoGe2O6 (+20.1 K) and CaNiGe2O6 (?13.4 K), suggesting an altered interplay between the concurring AFM and FM interaction in and between the M1 chains. CaMnGe2O6 finally shows an AFM ordering below 11 K. Here the magnetic moments are mainly oriented along the a-axis with a small tilt out from the a–c plane.
机译:已通过水热或陶瓷烧结技术合成了化合物CaFeSi2O6(钙铁矿),CaNiGe2O6,CaCoGe2O6和CaMnGe2O6,随后通过SQUID磁法和粉末中子衍射对其进行了表征,以确定低温下的磁性和自旋结构。所有这四种化合物均显示出众所周知的斜单环结构类型,具有单斜晶对称性,在所有研究温度下的空间群为C2 / c,Z = 4。低于35 K的水辉石在边缘共享八面体的无限M1链中显示出自旋的铁磁(FM)耦合。 FM耦合支配着相邻链之间的反铁磁(AFM)耦合。磁矩位于a–c平面内,并且与晶体学a轴形成43°角。 CaFeSi2O6中的磁有序性导致通过磁相变的晶格参数,Fe–O键长和原子间Fe–Fe距离显着不连续,这可以从粉末中子衍射数据的Rietveld改进中检测到。 CaCoGe2O6和CaNiGe2O6在18 K以下显示磁有序,自旋结构类似于菱锰矿中的自旋结构,其中M1链之间具有FM耦合且自旋是AFM耦合。力矩在交流平面内。但是,顺磁性居里温度从CaFeSi2O6(+40.2 K)降至CaCoGe2O6(+20.1 K)和CaNiGe2O6(?13.4 K)降低,表明在M1链中和M1链之间同时发生的AFM和FM相互作用之间的相互作用发生了改变。 CaMnGe2O6最终显示出低于11 K的AFM顺序。此处,磁矩主要沿a轴定向,并且从ac平面向外倾斜很小。

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