首页> 外文OA文献 >Frustrated antiferromagnetic spin chains of edge-sharing tetrahedra in volcanic minerals K3Cu3(Fe0.82Al0.18)O2(SO4)4 and K4Cu4O2(SO4)4MeCl
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Frustrated antiferromagnetic spin chains of edge-sharing tetrahedra in volcanic minerals K3Cu3(Fe0.82Al0.18)O2(SO4)4 and K4Cu4O2(SO4)4MeCl

机译:边缘共享四面体的挫折反铁磁自旋链   火山矿物K3Cu3(Fe0.82al0.18)O2(sO4)4和K4Cu4O2(sO4)4meCl

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摘要

The calculation of the sign and strength of magnetic interactions in twononcentrosymmetric minerals (klyuchevskite, K3Cu3(Fe0.82Al0.18)O2(SO4)4 andpiipite, K4Cu4O2(SO4)4Cu0.5Cl) has been performed based on the structural data.As seen from the calculation results, both minerals comprisequasi-one-dimensional frustrated antiferromagnets. They contain frustrated spinchains from edge-sharing Cu4 tetrahedra with strong antiferromagnetic couplingswithin chains and very weak ones between chains. Strong frustration of magneticinteractions is combined with the presence of the electric polarization intetrahedra chains in piipite. The uniqueness of magnetic structures of theseminerals caused by peculiarities of their crystal structures has beendiscussed. Keywords: Frustrated quasi-one-dimensional antiferromagnets,tetrahedral spin chains, klyuchevskite K3Cu3(Fe0.82Al0.18)O2(SO4)4, piypiteK4Cu4O2(SO4)4MeCl
机译:根据结构数据计算了两种非中心对称矿物(斜质硅铁矿,K3Cu3(Fe0.82Al0.18)O2(SO4)4和锂铁矿,K4Cu4O2(SO4)4Cu0.5Cl)的磁相互作用的符号和强度。从计算结果来看,两种矿物均包含准一维受挫反铁磁体。它们包含来自边缘共享的Cu4四面体的受阻自旋链,链中具有强反铁磁耦合,链之间具有非常弱的反铁磁耦合。磁性相互作用的强烈挫败感与在彼彼特石中的四面体链中存在电极化有关。讨论了由矿物晶体结构的特殊性引起的磁性结构的独特性。关键词:沮丧的准一维反铁磁体四面体自旋链斜硅钙石K3Cu3(Fe0.82Al0.18)O2(SO4)4,piypiteK4Cu4O2(SO4)4MeCl

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