Structure refinement and magnetic properties of synthetic Co3Ge2O5(OH)4 phyllogermanate

被引:3
作者
Belskaya, N. A. [1 ,4 ]
Khrapova, E. K. [1 ]
Ivanova, A. A. [1 ]
Eremin, E. V. [2 ,3 ]
Pavlov, S. I. [1 ]
Krasilin, A. A. [1 ]
机构
[1] Ioffe Inst, Polytech Skaya St 26, St Petersburg 194021, Russia
[2] Kirensky Inst Phys, Akademgorodok 50,Bld 38, Krasnoyarsk 660036, Russia
[3] Reshetnev Siberian State Univ Sci & Technol, 31 Krasnoyarsky Rabochy Ave, Krasnoyarsk 660037, Russia
[4] Ioffe Inst, Lab New Inorgan Mat, Polytech Skaya St 26, St Petersburg 194021, Russia
基金
俄罗斯科学基金会;
关键词
Layered material; Lizardite structure; Hydrothermal synthesis; Crystal structure; Rietveld method; Antiferromagnetism/Ferromagnetism; HYDROTHERMAL SYNTHESIS; BOND-VALENCE; CHRYSOTILE; NANOTUBES; BEHAVIOR; MINERALS; PHASE; SIZE;
D O I
10.1016/j.jmmm.2023.171262
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Co3Ge2O5(OH)4 relates to a specific group of 1:1 layered compounds with an ability to form either platy or tubular particles depending on chemical composition. Despite successful synthesis and perspective ap-plication, there is a lack of information on its crystal structure and magnetic properties, granted by Co ions. Co3Ge2O5(OH)4 phyllogermanate nanoparticles have been obtained using a hydrothermal method and characterised using powder X-ray diffraction and magnetisation measurements. Triclinic symmetry with a 1:P1 space group has been established. The unit cell contains three layers perpendicular to the c crystallographic direction, with 7.6 angstrom spacing and -b/3 shift of the middle layer. At a low magnetic field of 100 Oe the compound undergoes a magnetic transition at TN = 5.2 K. The field of 9 T is not sufficient to take the sample to a magnetically saturated state with an asymptotic magnetic moment of 2.43 mu B/Co2+. The estimations of the intralayer and interlayer exchange constants give values of J1/kB = 2.75 K and J2/kB = 0.25 K, respectively.
引用
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页数:7
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