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Precipitation of magnetite from yttrium iron silicate glass

机译:钇铁硅酸盐玻璃中磁铁矿的沉淀

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Oxide glasses containing a large amount of rare earth elements show the Faraday effect [1-3], which is applicable to an optical isolator. However, these oxide glasses are paramagnetic at room tem-perature, and possess very low paramagnetic Curie temperatures [4,5], so that high external magnetic field must be applied to attain high magnetization and large Faraday rotation angle in these materials. In general, the random arrangement of magnetic moments in oxide glasses leads to a substantial descent of magnetic transition temperature [6]. In some cases, the correlation among magnetic mo-ments does not extend to the long range, but is restricted within magnetic clusters of finite size, and the frustration of magnetic moments occurs in the boundary region among clusters [7-12]. Such a magnetic structure makes the ferro- or ferrimagnetic order unstable. Therefore, ferro- and ferrimagnet-ism with high Curie temperatures hardly take place in oxide glasses. Nonetheless, glass is an attractive material because of ease of forming any shapes such as fibres and thin films. One way to produce high magnetization in oxide glass is to introduce huge magnetic moments such as magnetization vectors of ferro- or ferrimagnetic microcrystals. The incorpora-tion of magneto-optical microcrystals into glass is also useful for the construction of waveguides equipped with isolators. Magneto-optical properties of magnetic fine particles such as Ni, Co and Cd1_v.MnvTe incorporated into several matrices were reported recently [13-16]. Magnetite, Fe3O4, is one of the compounds which show large magneto-optical effects. The Verdet constant of Fe3O4 thin film was reported to be 2.2 rad A"1 for light with a wavelength of 632.8 nm [17]. Studies on the crystall-ization of Fe3O4 from sodium silicate [18] and calcium silicate [19] glasses have been carried out. Nonetheless, it is useful to examine other glass systems containing Fe3O4 particles from the view-point of preparation of new magneto-optical mater-ials. In the present investigation, an attempt was made to prepare yttrium silicate glass containing Fe3O4 particles by heat-treating yttrium iron silicate glass. The magnetic properties of the resultant materials are reported.
机译:包含大量稀土元素的氧化物玻璃具有法拉第效应[1-3],适用于光学隔离器。然而,这些氧化物玻璃在室温下是顺磁性的,并且具有非常低的顺磁性居里温度[4,5],因此必须施加高的外部磁场以在这些材料中获得高的磁化强度和大的法拉第旋转角。通常,氧化物玻璃中磁矩的随机排列会导致磁转变温度大幅下降[6]。在某些情况下,磁矩之间的相关性不会延伸到很远的范围,而是会限制在有限大小的磁簇中,并且磁矩的挫折会发生在簇之间的边界区域[7-12]。这样的磁性结构使得铁或亚铁磁性的次序不稳定。因此,在氧化物玻璃中几乎不会发生居里温度高的铁磁性和亚铁磁性。但是,由于易于形成任何形状,例如纤维和薄膜,玻璃是有吸引力的材料。在氧化物玻璃中产生高磁化强度的一种方法是引入巨大的磁矩,例如铁或亚铁磁微晶的磁化矢量。将磁光微晶结合到玻璃中也可用于构造配备隔离器的波导。最近报道了掺入几种基质中的磁性细颗粒如Ni,Co和Cd1_v.MnvTe的磁光特性[13-16]。磁铁矿Fe3O4是显示出较大的磁光效应的化合物之一。据报道,Fe3O4薄膜的Verdet常数对于波长为632.8 nm的光为2.2 rad A“1。[17]。研究了从硅酸钠[18]和硅酸钙[19]玻璃中结晶出Fe3O4的研究。然而,从制备新的磁光材料的角度来看,检查含Fe 3 O 4颗粒的其他玻璃体系是有用的。在本研究中,尝试制备含Fe 3 O 4颗粒的硅酸钇玻璃。通过热处理氧化钇铁硅酸盐玻璃,报道了所得材料的磁性。

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