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掺锂的 kagome 自旋液体化合物。

Li doped kagome spin liquid compounds.

机构信息

Department of Materials Science and Engineering, University of Utah, Salt Lake City, Utah 84112, USA.

出版信息

Phys Chem Chem Phys. 2018 Aug 22;20(33):21693-21698. doi: 10.1039/c8cp03219j.

Abstract

Herbertsmithite and Zn-doped barlowite are two compounds for experimental realization of two-dimensional kagome spin liquids. Theoretically, it has been proposed that charge doping a quantum spin liquid gives rise to exotic metallic states, such as high-temperature superconductivity. However, one recent experiment on herbertsmithite with successful Li-doping surprisingly showed an insulating state even under a heavily doped scenario, which cannot be explained by previous theories. Using first-principles calculations, we performed a comprehensive study on the Li intercalation doping effect of these two compounds. For the Li-doped herbertsmithite, we identified the optimized Li position at the Cl-(OH)3-Cl pentahedron site instead of the previously speculated Cl-(OH)3 tetrahedral site. With increasing Li doping concentration, saturation magnetization decreases linearly due to charge transfer from Li to Cu ions. Moreover, we found that Li forms chemical bonds with nearby (OH)- and Cl- ions, which lowers the surrounding chemical potential and traps electrons, as evidenced by the localized charge distribution, explaining the insulating behavior measured experimentally. Though a different structure from herbertsmithite, Zn-doped barlowite shows the same features upon Li doping. We conclude that Li doping this family of kagome spin liquids cannot realize exotic metallic states, and other methods should be further explored, such as element substitution with those having different valence electrons.

摘要

赫伯特斯密斯石和掺锌巴罗莱特是两种实验实现二维 kagome 自旋液体的化合物。理论上,已经提出在量子自旋液体中掺杂电荷会产生奇异的金属态,例如高温超导性。然而,最近对赫伯特斯密斯石的一项成功的锂掺杂实验令人惊讶地显示出绝缘状态,即使在重度掺杂的情况下也是如此,这无法用以前的理论来解释。我们使用第一性原理计算对这两种化合物的 Li 插层掺杂效应进行了全面研究。对于 Li 掺杂的赫伯特斯密斯石,我们确定了优化的 Li 位置在 Cl-(OH)3-Cl 五面体位点,而不是之前推测的 Cl-(OH)3 四面体位点。随着 Li 掺杂浓度的增加,由于 Li 向 Cu 离子的电荷转移,饱和磁化强度呈线性下降。此外,我们发现 Li 与附近的 (OH)-和 Cl-离子形成化学键,这降低了周围的化学势并捕获电子,这可以通过局域电荷分布来证明,这解释了实验测量到的绝缘行为。尽管 Zn 掺杂巴罗莱特的结构与赫伯特斯密斯石不同,但在 Li 掺杂时表现出相同的特征。我们得出结论,在这类 kagome 自旋液体中掺杂 Li 不能实现奇异的金属态,应该进一步探索其他方法,例如用具有不同价电子的元素替代。

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