Frequency-Dependent Attenuation and Velocity Characteristics of Magnetically Lossy Materials

N. Cassidy
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引用次数: 10

Abstract

In many situations, the magnetic properties of sub-surface materials are often considered unimportant when compared to their 'dielectric' characteristics (i.e., permittivity and conductivity). However, if significant amounts of magnetic minerals exist, such as magnetite, hematite, maghemite and/or iron in its free state, then the relaxation phenomena of these magnetically lossy particles can have an overriding effect on the complex effective permittivity spectrum of the material. In this paper, the effective permittivity, attenuation and propagation characteristics of a range of nano-to-micro scale quartz/magnetite mixtures are investigated with the aim of determining how lossy magnetic minerals affect the macroscopic properties of the material as a whole. In addition, the measured results are compared to popular 'dielectric-based' mixing models (such as the Complex Refractive Index Model CRIM) and the nature of the magnetic relaxation mechanisms is discussed from the aspect of composite mediums. Results indicate that even relatively small amounts of magnetite can have a considerable effect on both signal attenuation and wave propagation velocity and that the current range of mixing models are inadequate for the description of magnetically lossy mixtures.
磁性损耗材料的频率衰减和速度特性
在许多情况下,与“介电”特性(即介电常数和导电性)相比,亚表面材料的磁性通常被认为不重要。然而,如果存在大量的磁性矿物,如磁铁矿、赤铁矿、磁铁矿和/或处于自由状态的铁,那么这些磁性损耗粒子的弛豫现象会对材料的复杂有效介电常数谱产生压倒性的影响。本文研究了一系列纳米到微米尺度石英/磁铁矿混合物的有效介电常数、衰减和传播特性,目的是确定有耗磁性矿物如何影响整体材料的宏观性质。此外,将测量结果与流行的“基于介电的”混合模型(如复折射率模型CRIM)进行了比较,并从复合介质的角度讨论了磁弛豫机制的性质。结果表明,即使是相对少量的磁铁矿也会对信号衰减和波传播速度产生相当大的影响,并且目前的混合模型范围不足以描述磁性损耗混合物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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