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Carbothermal Reduction Nitridation of Fly Ash, Diatomite and Raw Illite: Formation of Nitride Powders with Different Morphology and Photoluminescence Properties

机译:粉煤灰,硅藻土和原伊灰石的Carbothotmal降低硝化:不同形态学和光致发光性能的氮化物粉末的形成

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摘要

Rare-earth-doped SiAlON and Si3N4 materials from aluminosilicate starting materials have been reported to show superior photoluminescence (PL) properties. Three different starting materials, including pulverized coal furnace fly ash, diatomite and raw illite, were used for synthesis of nitride materials. The phase and morphology evolution of these products were carefully monitored at the low temperature range of 1350 °C to 1450 °C by X-ray diffraction (XRD), scanning electronic microscopy (SEM) and Fourier-transform infrared spectroscopy (FT-IR). The PL properties of Eu-doped nitride products were also comparatively characterized. The results show that the type of starting material affects the phase composition and the photoluminescence properties of products. The existence of aluminum and alkali metals could effectively promote nitridation reactions. Aluminum in the starting materials led to the formation of different aluminum-rich nitride phases. Thus, β-SiAlON could be achieved at a much lower temperature (1350 °C) using raw illite or fly ash containing the proper amount of aluminum. Additionally, excess aluminum led to the formation of corundum and 15R-SiAlON. The products from pulverized coal furnace fly ash had more prismatic particles, and the products from diatomite had more fibrous particles. With the progress of the nitridation process, the fibers were increased, becoming longer and straighter, and the prismatic particles were more obvious. The presence of aluminum in the starting materials led to a blue shift in the photoluminescence spectrum.
机译:据报道,稀土掺杂的Sialon和来自硅铝酸盐原料的Si3N4材料显示出优异的光致发光(PL)性质。三种不同的起始材料,包括粉煤灰粉煤灰,硅藻土和未生烟灰,用于合成氮化物材料。通过X射线衍射(XRD),扫描电子显微镜(SEM)和傅立叶变换红外光谱(FT-IR),在1350℃至1450℃的低温范围内小心地监测这些产物的相位和形态的进化。(扫描电子显微镜(SEM)(FT-IR) 。 Eu掺杂氮化物产物的PL性能也表现得很媲美。结果表明,原料的类型影响产物的相组成和光致发光性质。铝和碱金属的存在可以有效促进氮化反应。原料中的铝导致形成不同的富含铝的氮化物相。因此,可以使用含有适量铝的原iltite或粉煤灰在更低的温度(1350℃)下实现β-Sialon。此外,过量的铝导致刚玉和15R-Sialon的形成。来自煤粉炉粉煤灰的产品具有更多棱柱形颗粒,来自硅藻土的产品具有更多的纤维状颗粒。随着氮化过程的进展,纤维增加,变得更长,更直,棱柱形颗粒更加明显。在起始材料中存在铝的存在导致光致发光光谱的蓝色偏移。

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