Epitaxy‐Driven Ferroelectric/Non‐Ferroelectric Polymorph Selection in an All‐Fluorite System

Author:

Barriuso Eduardo12ORCID,Jiménez Ricardo3ORCID,Langenberg Eric45ORCID,Koutsogiannis Panagiotis1ORCID,Larrea Ángel1ORCID,Varela Manuel56ORCID,Magén César17ORCID,Algarabel Pedro A.17ORCID,Algueró Miguel3ORCID,Pardo José A.128ORCID

Affiliation:

1. Instituto de Nanociencia y Materiales de Aragón Universidad de Zaragoza‐CSIC Zaragoza 50018 Spain

2. Departamento de Ciencia y Tecnología de Materiales y Fluidos Universidad de Zaragoza Zaragoza 50018 Spain

3. Instituto de Ciencia de Materiales de Madrid CSIC Cantoblanco Madrid 28049 Spain

4. Departament de Física de la Matèria Condensada Universitat de Barcelona Barcelona 08028 Spain

5. Institut de Nanociència i Nanotecnologia de la Universitat de Barcelona (IN2UB) Universitat de Barcelona Barcelona 08028 Spain

6. Departament de Física Aplicada Universitat de Barcelona Barcelona 08028 Spain

7. Departamento de Física de la Materia Condensada Universidad de Zaragoza Zaragoza 50009 Spain

8. Laboratorio de Microscopías Avanzadas Universidad de Zaragoza Zaragoza 50018 Spain

Abstract

AbstractFilms of ferroelectric hafnia have hitherto been deposited on electrodes with a non‐fluorite crystal structure. As a result, they are polycrystalline, contain fractions of non‐ferroelectric polymorphs or have poor crystal quality. Here, a strategy that circumvents all these limitations is shown. Seven nanometers‐thick epitaxial Hf0.5Zr0.5O2 (HZO) films are deposited directly on yttria‐stabilized zirconia (YSZ) single‐crystals. The fluorite structure of the whole system enables coherent epitaxy, while the substrate orientation induces polymorph‐selective growth, being the HZO films orthorhombic on YSZ(111) and monoclinic on YSZ(001). Besides, the YSZ substrate can play the role of a buried floating electrode under the appropriate measuring conditions (temperature and frequency) thanks to its thermally‐activated oxygen conductivity. Indeed, out‐of‐plane ferroelectric switching is confirmed in the orthorhombic HZO samples at 185 °C and 0.01 Hz frequency. This original approach avoids the need to deposit conducting bottom layers, allowing high‐quality orthorhombic hafnia to be obtained directly on the substrate and its ferroelectric nature to be studied. Moreover, it constitutes a case of ion‐driven ferroelectric switching, and thus gives support to the recently proposed relationship between ionic conductivity, and ferroelectricity in fluorite systems.

Funder

Agencia Estatal de Investigación

Publisher

Wiley

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