Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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Efimov, V.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (7/7 displayed)

  • 2015Evolution of electromechanical properties of Bi<inf>1</inf><inf>-</inf><inf>x</inf>Pr<inf>x</inf>FeO<inf>3</inf> solid solutions across the rhombohedral-orthorhombic phase boundary: Role of covalency14citations
  • 2014Temperature and composition-induced structural transitions in Bi <inf>1-x</inf> la (Pr)<inf>x</inf> FeO<inf>3</inf> ceramics35citations
  • 2014Phase coexistence in Bi<inf>1-x</inf> Pr <inf>x</inf> FeO<inf>3</inf> ceramics30citations
  • 2013Evolution of crystal structure and ferroic properties of La-doped BiFeO<inf>3</inf> ceramics near the rhombohedral-orthorhombic phase boundary73citations
  • 2013Electromechanical and magnetic properties of BiFeO<inf>3</inf>-LaFeO <inf>3</inf>-CaTiO<inf>3</inf> ceramics near the rhombohedral-orthorhombic phase boundary36citations
  • 2013Magnetic and structural phase transitions in La<inf>0.5</inf>Sr <inf>0.5</inf>CoO<inf>3-δ</inf> (0 ≤ δ &lt; 0.3) cobaltites21citations
  • 2011Isothermal structural transitions, magnetization and large piezoelectric response in Bi1-xLaxFeO3 perovskites141citations

Places of action

Chart of shared publication
Pushkarev, N. V.
1 / 2 shared
Sikolenko, V.
7 / 8 shared
Dziaugys, A.
1 / 1 shared
Troyanchuk, I. O.
6 / 13 shared
Kholkin, Andrei L.
7 / 435 shared
Karpinsky, D. V.
6 / 22 shared
Tovar, M.
3 / 5 shared
Efimova, E.
2 / 2 shared
Shur, V. Y.
1 / 43 shared
Salak, A. N.
1 / 7 shared
Willinger, M.
1 / 4 shared
Lobanovsky, L. S.
1 / 1 shared
Chobot, A. N.
1 / 1 shared
Ritter, C.
1 / 50 shared
Araujo, Jp
1 / 91 shared
Khomchenko, Va
1 / 14 shared
Kakazei, Gn
1 / 8 shared
Troyanchuk, Io
1 / 1 shared
Bushinsky, Mv
1 / 2 shared
Karpinsky, Dv
1 / 2 shared
Chart of publication period
2015
2014
2013
2011

Co-Authors (by relevance)

  • Pushkarev, N. V.
  • Sikolenko, V.
  • Dziaugys, A.
  • Troyanchuk, I. O.
  • Kholkin, Andrei L.
  • Karpinsky, D. V.
  • Tovar, M.
  • Efimova, E.
  • Shur, V. Y.
  • Salak, A. N.
  • Willinger, M.
  • Lobanovsky, L. S.
  • Chobot, A. N.
  • Ritter, C.
  • Araujo, Jp
  • Khomchenko, Va
  • Kakazei, Gn
  • Troyanchuk, Io
  • Bushinsky, Mv
  • Karpinsky, Dv
OrganizationsLocationPeople

article

Isothermal structural transitions, magnetization and large piezoelectric response in Bi1-xLaxFeO3 perovskites

  • Tovar, M.
  • Araujo, Jp
  • Efimov, V.
  • Sikolenko, V.
  • Khomchenko, Va
  • Kakazei, Gn
  • Troyanchuk, Io
  • Kholkin, Andrei L.
  • Bushinsky, Mv
  • Karpinsky, Dv
Abstract

We report on the discovery of an isothermal structural transition observed in Bi1-xLaxFeO3 (0.17 <= x <= 0.19) ceramics. At room temperature, an initially pure polar rhombohedral phase gradually transforms into a pure antipolar orthorhombic one. The polar phase can be recovered by annealing at T > 300 degrees C. In accordance with neutron powder diffraction data, an inverse isothermal antipolar-polar transition takes place at T > 300 degrees C, where the polar phase becomes more stable. The antipolar phase is characterized by a weak ferromagnetic state, whereas the polar phase has been obtained in a mixed antiferromagnet-weak ferromagnet state. The relatively low external pressure induces polar-antipolar transition, but there is no evidence of electric-field-driven antipolar-polar transition. The observed large local piezoelectric response is associated with structural instability of the polar phase, whereas local multistate piezoelectric loops can be related to the domain wall pinning effect.

Topics
  • perovskite
  • impedance spectroscopy
  • phase
  • annealing
  • magnetization