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International Journal of Science and Engineering

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篇名 Influence of Sintering Time on Complex Permeability for Polycrystalline La0.7Sr0.3MnO3 Manganite
卷期 6:2
並列篇名 燒結時間對鑭鍶錳氧複數磁導率的影響
作者 尤孝雯
頁次 027-036
關鍵字 鑭鍶錳氧複數磁導率燒結時間共振頻率磁壁位移La0.7Sr0.3MnO3complex permeabilitysintering timeresonance frequencydomain wall displacement
出刊日期 201610
DOI 10.6159/IJSE.2016.(6-2).03

中文摘要

因具有在低磁場下的巨磁阻抗(GMI)效應,鈣鈦礦結構的錳氧化物鑭勰錳氧(LSMO)近年來 成為製作射頻微波元件與磁量計可選用的材料之一。由於LSMO的GMI效應與複數磁導率在 磁場下的變化行為有關,吾人製作不同燒結時間的樣品,探討在外加磁場下LSMO複數磁導率 的行為。研究結果顯示,增加燒結時間雖然可提升樣品的磁導率,卻會因磁滯損耗與渦電流損耗 而造成品質因子下降。當外加直流磁場時,樣品磁導率急遽減少。8小時,16小時與24小時燒 結的樣品,在450 G的外加磁場下,複數磁導率實部變化率在50 kHz , 40 kHz與30 kHz顯現 -84% , -86%與-85%的極大數值,複數磁導率虛部變化率在260 kHz , 260 kHz與160 kHz顯現 -94% , -94%與-93%的極大數值。外加磁場也會造成共振頻率fr增加,當磁場大於50 G時,fr會隨磁場線性增加,這個特性可應用於製作LSMO磁量計。

英文摘要

Recently, peroviskite manganite La0.7Sr0.3MnO3 (LSMO) has spurred lots of research excitement due to the exhibition of low-field giant magnetoimpedance (GMI) effect. Since the GMI effect for mangnites originates mainly from the magnetic-field-induced change of complex permeability, we have fabricated LSMO toroidal inductors with different sintering time to investigate the field-induced behavior of complex permeability. All the measured spectra show relaxation character due to domain wall displacement. As the sintering time increases, the permeability increases; however, the resonance frequency fr and quality factor (Q factor) decreases. Under applied magnetic field Bdc, the permeability decreases. A giant field-induced change ratio of the real part for complex permeability dμ’/μ’ of -84%, -86% and -85% at 50 kHz, 40 kHz and 30 kHz are obtained under a very small field Bdc= 450 G for the 8 hr, 16 hr and 24 hr sintering samples. Besides, a huge field-induced change ratio of the imaginary part for complex permeability dμ’’/μ’’ of -94%, -94% and -93% at 260 kHz, 260 kHz and 160 kHz are found under Bdc =450 G for the 8 hr, 16 hr and 24 hr sintering samples. The value of fr increases with Bdc and a linearly dependence between fr and Bdc is observed above 50 G. Our measured results are useful in understanding the GMI behavior of LSMO manganites and fabrication of LSMO magnetometers.

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