Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy

Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics were studied using x-ray, neutron diffraction and magnetization techniques. All the samples crystallized in rhombohedral structure with space group R3c. The compounds exhibit antiferromagnetic (AFM) ordering at 300 K and no evidence of further structu...

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Main Authors: Manisha Rangi, Ashish Agarwal, Sujata Sanghi, Ripandeep Singh, S. S. Meena, A. Das
Format: Article
Language:English
Published: AIP Publishing LLC 2014-08-01
Series:AIP Advances
Online Access:http://dx.doi.org/10.1063/1.4893241
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author Manisha Rangi
Ashish Agarwal
Sujata Sanghi
Ripandeep Singh
S. S. Meena
A. Das
author_facet Manisha Rangi
Ashish Agarwal
Sujata Sanghi
Ripandeep Singh
S. S. Meena
A. Das
author_sort Manisha Rangi
collection DOAJ
description Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics were studied using x-ray, neutron diffraction and magnetization techniques. All the samples crystallized in rhombohedral structure with space group R3c. The compounds exhibit antiferromagnetic (AFM) ordering at 300 K and no evidence of further structural or magnetic transition was observed on lowering of temperature below it. The magnetic structure of these substituted compounds are found to be collinear G-type AFM structure as against the non collinear incommensurate magnetic structure reported in the case of parent compound. The moments on Fe at 6 K are aligned along the a-axis in the case of Ca-doped sample. With increase in the ionic radii of dopant, the moments are found to be aligned in the ac plane and the angle of tilt away from the a-axis increases. The observed change in the magnetic structure with substitution is attributed to the intrinsic structural distortion as evidenced by the change in the bond angle (Fe-O-Fe) and bond distances (Bi-O, Fe-O). It has been found that heterovalent substitution A2+ results in the formation of oxygen vacancies in the parent lattices as the possibility of Fe4+ ruled out by Mössbauer spectra recorded at room temperature. Higher value of remnant magnetization (0.4187 emu/g) and coercivity (4.7554kOe) is observed in Bi0.8Ba0.2FeO3 sample in comparison to other substituted samples revealing a strong correlation between ionic radii and magnetization.
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spelling doaj.art-6ecc31295bf94ae8923d6b989e4bbaa72022-12-22T02:29:10ZengAIP Publishing LLCAIP Advances2158-32262014-08-0148087121087121-1110.1063/1.4893241016408ADVCrystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopyManisha Rangi0Ashish Agarwal1Sujata Sanghi2Ripandeep Singh3S. S. Meena4A. Das5Department of Applied Physics, Guru Jambheshwar University of Science & Technology, Hisar-125001 (Haryana) IndiaDepartment of Applied Physics, Guru Jambheshwar University of Science & Technology, Hisar-125001 (Haryana) IndiaDepartment of Applied Physics, Guru Jambheshwar University of Science & Technology, Hisar-125001 (Haryana) IndiaSolid State Physics Division, Bhabha Atomic Research Centre, Mumbai-400 085, IndiaSolid State Physics Division, Bhabha Atomic Research Centre, Mumbai-400 085, IndiaSolid State Physics Division, Bhabha Atomic Research Centre, Mumbai-400 085, IndiaBi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics were studied using x-ray, neutron diffraction and magnetization techniques. All the samples crystallized in rhombohedral structure with space group R3c. The compounds exhibit antiferromagnetic (AFM) ordering at 300 K and no evidence of further structural or magnetic transition was observed on lowering of temperature below it. The magnetic structure of these substituted compounds are found to be collinear G-type AFM structure as against the non collinear incommensurate magnetic structure reported in the case of parent compound. The moments on Fe at 6 K are aligned along the a-axis in the case of Ca-doped sample. With increase in the ionic radii of dopant, the moments are found to be aligned in the ac plane and the angle of tilt away from the a-axis increases. The observed change in the magnetic structure with substitution is attributed to the intrinsic structural distortion as evidenced by the change in the bond angle (Fe-O-Fe) and bond distances (Bi-O, Fe-O). It has been found that heterovalent substitution A2+ results in the formation of oxygen vacancies in the parent lattices as the possibility of Fe4+ ruled out by Mössbauer spectra recorded at room temperature. Higher value of remnant magnetization (0.4187 emu/g) and coercivity (4.7554kOe) is observed in Bi0.8Ba0.2FeO3 sample in comparison to other substituted samples revealing a strong correlation between ionic radii and magnetization.http://dx.doi.org/10.1063/1.4893241
spellingShingle Manisha Rangi
Ashish Agarwal
Sujata Sanghi
Ripandeep Singh
S. S. Meena
A. Das
Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy
AIP Advances
title Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy
title_full Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy
title_fullStr Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy
title_full_unstemmed Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy
title_short Crystal structure and magnetic properties of Bi0.8A0.2FeO3 (A = La, Ca, Sr, Ba) multiferroics using neutron diffraction and Mossbauer spectroscopy
title_sort crystal structure and magnetic properties of bi0 8a0 2feo3 a la ca sr ba multiferroics using neutron diffraction and mossbauer spectroscopy
url http://dx.doi.org/10.1063/1.4893241
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