Ferrimagnetic and metamagnetic layered cobalt (II)-hydroxides: first observation of a coercive field greater than 5 T

被引:73
作者
Kurmoo, M [1 ]
机构
[1] Inst Phys Chim & Mat Strasbourg, F-67037 Strasbourg, France
来源
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES | 1999年 / 357卷 / 1762期
关键词
cobalt; magnet; layer; clay; hydroxide;
D O I
10.1098/rsta.1999.0480
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The synthesis, characterization by XRD, UV-vis, IR and TGA and the magnetic properties of four layered compounds, namely 1 Co-5(OH)(8)(H2O)(2)(NO3)(2); 2 Co-5(OH)(8)(O2CC6H4CO2) . 2H(2)O; 3 Co-2(OH)(3)(NO3); 4 Co-4(OH)(2)(O2CC6H4CO2)(3) . (NH3)(1.5)(H2O)(2.5), are reported. 1 and 2 are characterized by triple-deck layers consisting of both octahedral and tetrahedral cobaltous ions and 3 and 4 contain single-deck layers of only octahedral cobaltous ions. I and 2 behave as ferrimagnets which are characterized by a minimum in the chi T versus T plot, spontaneous magnetization, imaginary AC-susceptibility and hysteresis loop. The Curie temperatures are 30 and 40 K and the coercive fields at 4.2 K are 850 and 1750 Oe, respectively. 3 and 4 behave as metamagnets which are characterized by maxima in the susceptibility at the Neel temperature of 10 and 38 K, respectively, and by a critical field (antiferromagnetic <-> paramagnetic) of ca. 1 kOe for 3 at 4.5 K and greater than 50 kOe for 4 at 2 K. The tricritical temperature, separating the region of reversible and non-reversible M versus H, for 4 is established at 22.5 K. The long-range magnetic ordering for the two structural types is discussed on the basis of dipolar interactions between layers. The intralayer interactions are ferromagnetic in all cases whereas the interlayer interactions are ferromagnetic for 1 and 2 and antiferromagnetic for 3 and 4. The results indicate that the Curie or Neel temperature is weakly dependent on the interlayer distance and its observation does not depend on the existence of covalent bonds between the layers. The large coercive fields observed are due to the alignment of the moments perpendicular to the layers and the synergy between crystalline shape and single-ion anisotropies.
引用
收藏
页码:3041 / 3061
页数:21
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