Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films

Perovskite manganites are viewed as one of the key building blocks of oxide spintronics devices due to their attractive physical properties. However, cation off-stoichiometry at epitaxial interfaces between manganites and other materials can lead to interfacial dead layers, severely reducing the dev...

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Main Authors: Li, Zhi Peng, Bosman, Michel, Yang, Zhen, Ren, Peng, Wang, Lan, Zhu, Weiguang, Dong, Zhili, Foo, Yong Lim, Cao, Liang, Yu, Xiaojiang, Ke, Chang, Breese, Mark B. H., Rusydi, Andrivo
Other Authors: School of Electrical and Electronic Engineering
Format: Article
Language:English
Published: 2013
Online Access:https://hdl.handle.net/10356/97277
http://hdl.handle.net/10220/10426
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-972772020-06-01T10:13:48Z Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films Li, Zhi Peng Bosman, Michel Yang, Zhen Ren, Peng Wang, Lan Zhu, Weiguang Dong, Zhili Foo, Yong Lim Cao, Liang Yu, Xiaojiang Ke, Chang Breese, Mark B. H. Rusydi, Andrivo School of Electrical and Electronic Engineering School of Materials Science & Engineering School of Physical and Mathematical Sciences Perovskite manganites are viewed as one of the key building blocks of oxide spintronics devices due to their attractive physical properties. However, cation off-stoichiometry at epitaxial interfaces between manganites and other materials can lead to interfacial dead layers, severely reducing the device performance. Here, transmission electron microscopy and synchrotron-based spectroscopy are used to demonstrate that oxygen vacancies during growth serve as a critical factor for modifying the cation stoichiometry in pulsed laser deposited La0.8Sr0.2MnO3 films. Near the film/substrate (SrTiO3) interface, A-site cations (La/Sr) are in excess when oxygen vacancies are induced during film growth, partially substituting Mn. Simultaneously, Sr cations migrate towards the film surface and form a SrO rock-salt monolayer. Consequentially, a gradient of the Mn nominal valence is observed along the film growth direction, leading to anomalous magnetic properties. The results narrow the selection range of useful oxygen pressures during deposition and demonstrate that accurate cation stoichiometry can only be achieved after oxygen vacancies are eliminated during growth. This finding suggests that the oxygen pressure serves as a tuning parameter for the interfacial dead layers and, hence, for control over device properties. 2013-06-17T03:49:19Z 2019-12-06T19:40:50Z 2013-06-17T03:49:19Z 2019-12-06T19:40:50Z 2012 2012 Journal Article Li, Z., Bosman, M., Yang, Z., Ren, P., Wang, L., Cao, L., et al. (2012). Interface and Surface Cation Stoichiometry Modified by Oxygen Vacancies in Epitaxial Manganite Films. Advanced Functional Materials, 22(20), 4312-4321. 1616-3028 https://hdl.handle.net/10356/97277 http://hdl.handle.net/10220/10426 10.1002/adfm.201200143 en Advanced functional materials © 2012 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim.
institution Nanyang Technological University
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language English
description Perovskite manganites are viewed as one of the key building blocks of oxide spintronics devices due to their attractive physical properties. However, cation off-stoichiometry at epitaxial interfaces between manganites and other materials can lead to interfacial dead layers, severely reducing the device performance. Here, transmission electron microscopy and synchrotron-based spectroscopy are used to demonstrate that oxygen vacancies during growth serve as a critical factor for modifying the cation stoichiometry in pulsed laser deposited La0.8Sr0.2MnO3 films. Near the film/substrate (SrTiO3) interface, A-site cations (La/Sr) are in excess when oxygen vacancies are induced during film growth, partially substituting Mn. Simultaneously, Sr cations migrate towards the film surface and form a SrO rock-salt monolayer. Consequentially, a gradient of the Mn nominal valence is observed along the film growth direction, leading to anomalous magnetic properties. The results narrow the selection range of useful oxygen pressures during deposition and demonstrate that accurate cation stoichiometry can only be achieved after oxygen vacancies are eliminated during growth. This finding suggests that the oxygen pressure serves as a tuning parameter for the interfacial dead layers and, hence, for control over device properties.
author2 School of Electrical and Electronic Engineering
author_facet School of Electrical and Electronic Engineering
Li, Zhi Peng
Bosman, Michel
Yang, Zhen
Ren, Peng
Wang, Lan
Zhu, Weiguang
Dong, Zhili
Foo, Yong Lim
Cao, Liang
Yu, Xiaojiang
Ke, Chang
Breese, Mark B. H.
Rusydi, Andrivo
format Article
author Li, Zhi Peng
Bosman, Michel
Yang, Zhen
Ren, Peng
Wang, Lan
Zhu, Weiguang
Dong, Zhili
Foo, Yong Lim
Cao, Liang
Yu, Xiaojiang
Ke, Chang
Breese, Mark B. H.
Rusydi, Andrivo
spellingShingle Li, Zhi Peng
Bosman, Michel
Yang, Zhen
Ren, Peng
Wang, Lan
Zhu, Weiguang
Dong, Zhili
Foo, Yong Lim
Cao, Liang
Yu, Xiaojiang
Ke, Chang
Breese, Mark B. H.
Rusydi, Andrivo
Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
author_sort Li, Zhi Peng
title Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
title_short Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
title_full Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
title_fullStr Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
title_full_unstemmed Interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
title_sort interface and surface cation stoichiometry modified by oxygen vacancies in epitaxial manganite films
publishDate 2013
url https://hdl.handle.net/10356/97277
http://hdl.handle.net/10220/10426
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