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arXiv 0811.1386cond-mat.mtrl-sci
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A位磁性尖晶石CoAl $_{2-x}$ Ga $_x$ O $_4$金刚石晶格上的磁阻挫调谐:晶格膨胀和位序无序

Tuning magnetic frustration on the diamond lattice of the A-site magnetic spinels CoAl$_{2-x}$Ga$_x$O$_4$: Lattice expansion and site disorder

Brent C. Melot, Katharine Page, Ram Seshadri, E. M. Stoudenmire, Leon Balents, Doron L. Bergman, Thomas Proffen

摘要:

在金刚石晶格A位上具有磁性Co $^{2+}$离子的尖晶石CoB $_2$ O $_4$可能由于竞争的近邻($J_1$)和次近邻($J_2$)相互作用而受到阻碍。在这里,我们描述了尝试调整这些相互作用的相对强度的非磁性B-网站上的取代。我们采用的系统是CoAl $_{2-x}$ Ga $_x$ O $_4$,其中Al被较大的Ga系统地取代,表面上在B位点上。正如预期的那样,Ga取代使晶格膨胀,导致A位上的Co原子彼此被推得更远,从而削弱了磁相互作用。此外,Ga以浓度依赖性方式分布在B和A位点之间,随着$x$的增加,从A位点置换越来越多的Co。这种增加的反转,这是在室温下进行的中子衍射研究证实,影响磁有序非常显着,并改变了基态的性质。磁耦合的建模说明了由阳离子位点无序引起的复杂性。

英文摘要:

The spinels CoB$_2$O$_4$ with magnetic Co$^{2+}$ ions on the diamond lattice A site can be frustrated because of competing near-neighbor ($J_1$) and next-near neighbor ($J_2$) interactions. Here we describe attempts to tune the relative strengths of these interactions by substitution on the non-magnetic B-site. The system we employ is CoAl$_{2-x}$Ga$_x$O$_4$, where Al is systematically replaced by the larger Ga, ostensibly on the B site. As expected, Ga substitution expands the lattice, resulting in Co atoms on the A-site being pushed further from one other and thereby weakening magnetic interactions. In addition, Ga distributes between the B and the A site in a concentration dependent manner displacing an increasing amount of Co from the A site with increasing $x$. This increased inversion, which is confirmed by neutron diffraction studies carried out at room temperature, affects magnetic ordering very significantly, and changes the nature of the ground state. Modeling of the magnetic coupling illustrates the complexity that arises from the cation site disorder.

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