钙钛矿晶体结构双氧化物复介电常数的表征

J. A. Mergos, J. Daskalakis, C. Dervos
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引用次数: 3

摘要

钙钛矿的矿物结构是立方的,每单位细胞有一个公式重量。它的名字是由矿物CaTiO3命名的。大量的双氧化物(以及一些碘酸盐和双卤化物)被归类为属于这种类型。本文介绍了钙钛矿晶体的介电特性,即复介电常数(实部和虚部)和损耗因子(tan δ)。在20 Hz-1 MHz频率范围内,用等效电容-电导并联电路法得到了它们的值。将TiO2(主要为锐钛矿结构)和CaCO3(方解石)粉末混合,单轴压缩成球团制备样品。这些都是在高达1200摄氏度的温度下烧结的。XRD结果表明,锐钛矿不仅转化为金红石,方解石转化为石灰(CaO),而且形成了与天然钙钛矿一样的双氧化物CaTiO3。与钙钛矿结构强度较低的低温烧结样品相比,它的形成与较高的介电常数值和显着降低的损耗有关。这种高k和低损耗的介电材料最近在寻求电信应用的智能天线方面受到了极大的关注
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Complex permittivity characterization of double oxides of the perovskite crystal structure
Perovskite mineral structure is cubic, with one formula-weight per unit cell. Its name was given by the mineral CaTiO3. A large number of double oxides (as well as some iodates and double halides) are classified as belonging to this type. In this work the dielectric properties of perovskite crystals are presented, namely the complex permittivity (real and imaginary part) and the loss factor (tan delta). Their values in the 20 Hz-1 MHz frequency range were obtained using the equivalent capacitance-conductance parallel circuit method. Specimens were prepared by mixing TiO2 (of predominantly anatase structure) and CaCO3 (calcite) powders and compressing them uniaxially to form pellets. These were sintered at temperatures as high as 1200 degC. According to the XRD results obtained, not only did the anatase convert to rutile and the calcite to lime (CaO), but also the double oxide CaTiO3 was formed, as in the natural perovskite mineral. Its formation was related to higher dielectric constant values and significantly lower losses compared to specimens sintered at lower temperatures, where the perovskite structure was less intense. Such high-K and low-loss dielectric materials have lately found significant attention in the quest of smart antennas for telecommunication applications
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