(111)取向受挫量子焦绿石薄膜的外延稳定性

Fangdi Wen, Tsung-Chi Wu, Xiaoran Liu, M. Terilli, M. Kareev, J. Chakhalian
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引用次数: 1

摘要

受挫稀土焦绿钛酸盐Yb$_2$Ti$_2$O$_7$和Tb$_2$Ti$_2$O$_7$被认为是实现量子自旋冰(QSI)的有希望的候选材料。多个奇异量子相,包括库仑铁磁体、量子价键固体和四极有序,已经被预测在(111)定向外磁场的应用下出现在QSI状态。在这里,我们报道了沿(111)方向,R$_2$Ti$_2$O$_7$ (R = Er, Yb和Tb)的受挫量子焦绿石超薄膜的初步成功的逐层生长。我们通过原位RHEED, x射线衍射,互反空间映射和x射线光电子能谱等方法证实了它们的高结晶度和适当的化学成分。具有平面几何结构的大面积(111)定向QSI结构的可用性为块状平台提供了新的补充,以探索准二维极限下的应变和磁场依赖性质。
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Epitaxial stabilization of (111)-oriented frustrated quantum pyrochlore thin films
Frustrated rare-earth pyrochlore titanates, Yb$_2$Ti$_2$O$_7$, and Tb$_2$Ti$_2$O$_7$ have been proposed as promising candidates to realize quantum spin ice (QSI). Multiple exotic quantum phases, including Coulombic ferromagnet, quantum valence-bond solid, and quadrupolar ordering, have been predicted to emerge in the QSI state upon application of a (111)-oriented external magnetic field. Here, we report on the primal successful layer-by-layer growth of ultra-thin films of frustrated quantum pyrochlores, R$_2$Ti$_2$O$_7$ (R = Er, Yb, and Tb), along the (111) direction. We confirm their high crystallinity and proper chemical composition by a combination of methods, including in-situ RHEED, x-ray diffraction, reciprocal space mapping, and x-ray photoelectron spectroscopy. The availability of large area (111)-oriented QSI structures with planar geometry offers a new complementary to the bulk platform to explore strain and magnetic field dependent properties in the quasi-2D limit.
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