Abstract

Interaction of multiple oxidation states of manganese ions with rare earth ions in manganites leads to the observation of various magnetic ground states. To understand the effect of average ionic size on electrical conductivity and magnetic ground state properties in Dy1-xKxMnO3 (x=0.0, 0.1, 0.2 & 0.3), we have investigated electron transport as a function of temperature and magnetic properties as a function of temperature, frequency and magnetic field of these compounds. Although mixed valent manganese ions can facilitate a double exchange interaction via oxygen ion leading to a ferromagnetic metallic ground state, no insulator-metal transition was detected. On the other hand, in the compounds with x=0.0 to 0.2, transport properties suggested an adiabatic small polaron hopping conduction mechanism. However, x=0.3 compound followed a variable range hopping conduction. Temperature variation of magnetization data exhibited three different types of transitions involving Mn and Dy ions. The bifurcation between zero field cooled and field cooled magnetization data was observed in all the compounds. Field-dependent magnetization of all the compounds showed hysteresis loops for temperatures less than 10 K. Although large irreversibility between zero field cooled and field cooled magnetization data was observed with a peak for x=0.3, the peak temperatures did not alter with frequency ruling out the possibility of spin glass behavior. The presence of hysteresis loops and lack of saturation magnetization implied the simultaneous presence of ferromagnetic and antiferromagnetic exchange interactions well within the antiferromagnetic ordering of Mn ions.

Highlights

  • The powder X-ray diffraction data of DMO along with lattice parameters are reported in International Centre for Diffraction Data (ICDD), 2016.24 Structural distortions due to the movement of oxygen ions towards the centre of manganese oxide octahedra as observed in the pure oxide, DMO were attributed to the smaller Dy ion at A-site in ABO3 (A: transition/rare earth metal, B: transition/alkaline earth metal ion) perovskites and Jahn-Teller (JT) distortions caused due to Mn3+ ions

  • It is well known that Double Exchange (DE) interaction between Mn3+ and Mn4+ ions through an oxygen ion is responsible for ferromagnetic metallic properties.[12]

  • The ρ(T) of DMO, Dy0.9K0.1MnO3 & Dy0.8K0.2MnO3 have attributed to Small Polaron Hopping (SPH) conduction mechanism since Mn3+ electrons are the majority of charge carries in these compounds

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Summary

INTRODUCTION

RSG state has been identified in YMnO313 and K (potassium) doped NdMnO3.18 Another class of spin glass behavior known as Cluster Spin Glass[19,20] has been observed in compounds where spins are arranged in the form of clusters inside ferromagnetic domains. The origin of such diverse magnetic states in manganites stems from the arrangement of magnetic spins in the lattice and their response to an external magnetic field as a function of temperature. In view of the multi functional properties of these materials, we have undertaken monovalent ionic substitution at Dy site in DMO and carried out measurements of transport and magnetic properties of the new series of compounds in Dy1-xKxMnO3 whose structural properties were recently reported by us.[23]

EXPERIMENTAL DETAILS
Structure and transport studies
Magnetization studies
CONCLUSIONS
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