On the origin of oxygen isotope exchange induced ferroelectricity in strontium titanate

Hai Yao Denga, Chi Hang Lam, Haitao Huang

Research output: Journal article publicationJournal articleAcademic researchpeer-review

4 Citations (Scopus)

Abstract

The quantum paraelectric strontium titanate can be made ferroelectric through replacing oxygen atoms with their heavy isotopes. Although suppressed quantum fluctuations have been widely believed to be the origin, the details remain unsettled. The controveries are often framed using Barrett formula, which involves two quantities termed T0 and T1, respectively. The obervations can be equally explained by assuming either a decrease in T1 or an increase in T0 upon isotope replacement. The conventional view holds a direct connection between quantum fluctuations and the T1 and hence adopts the decreasing T1 picture. In this paper, we offer a different opinion, in which the T1 bears a different meaning and quantum fluctuations are attached to another quantity to be denoted 0. We show that a decrease in 0 could diminish quantum fluctuations and simultaneously enhance T0. A vibronic mechanism is presented as a possible route to the 0 change. The isotope effects are argued to be rather non-local. The dynamics of the system could be highly quasi-one-dimensional and this is then employed in discussing the relation between a soft mode and a recently observed central mode.
Original languageEnglish
Article number234
JournalEuropean Physical Journal B
Volume85
Issue number7
DOIs
Publication statusPublished - 1 Jul 2012

ASJC Scopus subject areas

  • Electronic, Optical and Magnetic Materials
  • Condensed Matter Physics

Cite this