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Improper ferroelectricity in lawsonite CaAl2Si2O7(OH)2·H2O: hysteresis and hydrogen ordering
E K H Salje1, S Crossley, S Kar-Narayan
1Department of Earth Sciences, University of Cambridge, Cambridge, UK.
Ferroelectricity in lawsonite ceramics is improper, driven by hydrogen ordering. Remanent polarization shows a near-linear temperature dependence, confirming this mechanism below the Curie temperature of 124 K.
Area of Science:
- Solid State Physics
- Materials Science
- Crystallography
Background:
- Ferroelectricity in ceramic materials is crucial for electronic applications.
- Understanding the mechanisms and temperature dependence of ferroelectric properties is key to material design.
- Lawsonite, a calcium aluminum silicate mineral, has recently shown potential ferroelectric properties.
Purpose of the Study:
- To investigate the ferroelectric hysteresis of ceramic lawsonite.
- To determine the temperature dependence of its remanent polarization.
- To elucidate the nature and driving mechanism of the ferroelectric phase transition in lawsonite.
Main Methods:
- Ferroelectric hysteresis measurements on ceramic lawsonite.
- Analysis of temperature-dependent remanent polarization (P(r)).
- Thermodynamic analysis of the phase transition (Pmcn-P 2(1)cn) using the order parameter (Q).
Main Results:
- Remanent polarization P(r) exhibits a temperature dependence described by P(r) = P(o)Θ(s)(cothΘ(s)/T - cothΘ(s)/T(c)) with Θ(s) = 26 K.
- The observed almost linear temperature evolution of P(r) indicates improper ferroelectricity.
- The Curie temperature (T(c)) was determined to be 124 K, and the phase transition is strictly continuous.
Conclusions:
- The ferroelectricity in lawsonite ceramics is confirmed to be improper.
- Hydrogen ordering is identified as the primary driving mechanism for the ferroelectric phase transition.
- The findings provide insights into the fundamental properties of ferroelectric phase transitions in silicate minerals.
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