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Exchange Interaction and $T_c$ in Alkaline-earth-metal-oxide-based DMS without Magnetic Impurities: First Principle Pseudo-SIC and Monte Carlo Calculation

机译:基于碱土金属氧化物的Dms中的交换相互作用和$ T_c $   没有磁杂质:第一原理伪sIC和蒙特卡罗   计算

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摘要

The prospects of half-metallic ferromagnetism being induced by theincorporation of C atoms into alkaline-earth-metal-oxides are investigated bythe first principle calculation. The origin of the ferromagnetism is discussedthrough the calculation of the electronic structure and exchange couplingconstant by using the pseudo-potential-like self-interaction-corrected localspin density method. The Curie temperature ($T_c$) is also predicted byemploying the Monte Carlo simulation. It is shown that by taking the electronself-interaction into account, the half-metallic ferromagnetism induced by C inthe host materials is more stabilized in comparison with the standard LDA case,and the C's $2p$ electron states in the bandgap become more localized resultingin the predominance of the short-ranged exchange interaction. While theferromagnetism in MgO$_{1-x}$C$_x$ is stabilized due to the exchangeinteraction of the $1st$-nearest neighbor pairs and might be suppressed by theanti-ferromagnetic super-exchange interaction at higher $x$, the ferromagnetismin CaO$_{1-x}$C$_x$, SrO$_{1-x}$C$_x$, and BaO$_{1-x}$C$_x$ is stabilized byboth the $1st$- and $2nd$-nearest neighbor pairs, and $T_c$ monotonouslyincreases with the C concentration.
机译:通过第一性原理计算,研究了将碳原子掺入碱土金属氧化物中诱发的半金属铁磁性的前景。通过电子结构的计算和利用伪势似自相互作用校正的局部自旋密度方法,计算了交换磁常数,讨论了铁磁性的起源。居里温度($ T_c $)也可以通过蒙特卡罗模拟来预测。结果表明,与标准的LDA情况相比,考虑到电子自身的相互作用,C在主体材料中诱导的半金属铁磁性更加稳定,并且带隙中的C的$ 2p $电子态变得更加局部化。短距离交换互动的优势。尽管MgO $ _ {1-x} $ C $ _x $中的铁磁性由于$ 1st $-最近邻居对之间的交换相互作用而得以稳定,并可能在$ x $较高的情况下被反铁磁超交换相互作用所抑制,钙铁蛋白CaO $ _ {{1-x} $ C $ _x $,SrO $ _ {1-x} $ C $ _x $和BaO $ _ {1-x} $ C $ _x $被第1个稳定-和$ 2 $-最近的邻居对,以及$ T_c $随着C浓度单调增加。

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