Abstract
The present work report synthesis of four-layer Aurivillius compound with systematic replacement of A-site Bi\(^{3+}\) cation via La\(^{3+}\). Four-layer Aurivillius structure and phase purity is confirmed by x-ray diffraction measurements. Raman spectroscopy measurement indicate that La replaces Bi from perovskite like slab. M\(\ddot{o}\)ssbauer spectroscopy measurement shows the presence of paramagnetic behaviour at room temperature and confirms the presence of Fe\(^{3+}\) in octahedral environment. Further, magnetization measurements indicate paramagnetic nature down to 5K similar to parent compound (Bi\(_5\)FeTi\(_3\)O\(_{15}\)) and suggest La substitution at A-site does not induce the magnetic ordering.
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Acknowledgements
Authors thank Dr. V G Sathe and Mr. Ajay Rathore for room temperature Raman spectroscopy measurement. DP thank Mr. Anil Gome and Dr. Ganesh Bera for help during XRD and dielectric measurements. We thank Dr. Rajeev Rawat and Suman Karmakar for magnetization measurements. DP thank Dr. Uday P. Deshpande for XPS measurements.
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Deepak Prajapat: Investigation, Data curation and analysis, Writing original manuscript. Akash Surampalli: Formal analysis, Manuscript review. V. Raghavendra Reddy: Conceptualization, Supervision, Manuscript review and editing.
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Prajapat, D., Surampalli, A. & Reddy, V.R. Study of La substituted four-layer Aurivillius compound Bi\(_5\)FeTi\(_3\)O\(_{15}\). Hyperfine Interact 244, 15 (2023). https://doi.org/10.1007/s10751-023-01826-5
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DOI: https://doi.org/10.1007/s10751-023-01826-5