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Thermal and morphological characterization of basalt continuous fibers

机译:玄武岩连续纤维的热学和形貌表征

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摘要

The basalts are abundant volcanic rocks formed from extensive wastes. The technology of continuous wiring produces basalt filaments in micrometric amorphous long fibers. In this work are presented results of the thermal and morphologic characterization of micrometric basalt fibers. These fibers showed excellent thermal stability, resulting in low weight change (less than 1 wt.%) up to 1000 ºC, under heating in inert or oxidant atmosphere. On the other hand, partial crystallization of basalt fibers occurred at ~ 800 ºC, resulting in diffraction peaks in the X-ray patterns, characteristic of silicates and aluminosilicates as the anorthite from the plagioclase class. The morphology of fibers after heating at 1000 ºC was changed due to the fusion and crystallization of the present phases.
机译:玄武岩是由大量废物形成的丰富的火山岩。连续布线技术可在微米级非晶长纤维中生产玄武岩长丝。在这项工作中提出了微米级玄武岩纤维的热学和形态学表征的结果。这些纤维表现出出色的热稳定性,在惰性或氧化剂气氛中加热时,在高达1000ºC的条件下,重量变化很小(小于1 wt。%)。另一方面,玄武岩纤维的部分结晶在〜800ºC发生,导致X射线衍射图出现衍射峰,这是斜长石类钙长石的硅酸盐和铝硅酸盐的特征。由于当前相的熔融和结晶,在1000℃加热后纤维的形态发生了变化。

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