Selective doping Barlowite for quantum spin liquid: a first-principles study
Abstract
Barlowite Cu4(OH)6FBr is a newly found mineral containing Cu2+ kagome planes. Despite similarities in many aspects to Herbertsmithite Cu3Zn(OH)6Cl2, the well-known quantum spin liquid (QSL) candidate, intrinsic Barlowite turns out not to be a QSL, possibly due to the presence of Cu2+ ions in between kagome planes that induce interkagome magnetic interaction [PRL, 113, 227203 (2014)]. Using first-principles calculation, we systematically study the feasibility of selective substitution of the interkagome Cu ions with isovalent nonmagnetic ions. Unlike previous speculation of using larger dopants, such as Cd2+ and Ca2+, we identify the most ideal stoichiometric doping elements to be Mg and Zn in forming Cu3Mg(OH)6FBr and Cu3Zn(OH)6FBr with the highest site selectivity and smallest lattice distortion. The equilibirium anti-site disorder in Mg/Zn- doped Barlowite is estimated to be one order of magnitude lower than that in Herbertsmithite. The single-electron band structure and orbital component analysis show that the proposed selective doping effectively mitigates the difference between Barlowite and Herbertsmithite.
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