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    Effect of hydrostatic pressure on modulated phases in Rb2ZnBr4

    K. Parlinski

    R. Currat and C. Vettier

    I. P. Aleksandrova

    G. Eckold

    • Institut Laue-Langevin, 156X Centre de Tri, 38042 Grenoble, France
    • Institute of Nuclear Physics, ul. Radzikowskiego 152, 31-342 Cracow, Poland

    • Institut Laue-Langevin, 156X Centre de Tri, 38042 Grenoble, France

    • L. V. Kirensky Institute of Physics, 660036 Krasnoyarsk, U.S.S.R.

    • Institut für Kristalographie, Rheinisch-Westfälische Technische Hochschule Aachen, Aachen, Federal Republic of Germany
    • Institut für Festkörperforschung, Kernforschungsanlage Jülich G.m.b.H., Jülich D-5170, Federal Republic of Germany

    Phys. Rev. B 46, 106 – Published 1 July, 1992

    DOI: https://doi.org/10.1103/PhysRevB.46.106

    Abstract

    Neutron-diffraction studies on modulated Rb2ZnBr4, carried out under hydrostatic pressure, revealed two new commensurate phases characterized by wave vectors q=2/7b* and q=1/4b*, respectively. The first-order phase transition between them is revealed by the coexistence of two distinct peaks in the diffraction pattern. The observed pressure-temperature phase diagram contains the above-mentioned phases, the ferroelectric commensurate phase q=1/3, and a region characterized by wave-vector values in the interval q=2/7– 1) / 3 . In this region the modulation wave vector exhibits stepwise behavior as a function of pressure but remains nearly constant in temperature runs. We have found in this region a characteristic memory effect in which two temperature runs performed at the same pressure lead to two different modulation wave-vector values, while only the thermal history of the sample is different in the two runs. At ambient pressure we confirm the presence of a multipeaked diffraction pattern just above the lock-in transition to the commensurate q=1/3 phase. At 122 K the phase transition from the 1/3 phase to the 1/4 phase is detected in pressure scans. The transition mechanism involves the q=2/7 phase, at least as a metastable intermediate phase.

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