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In situ ultrasonic diagnostic of zeolite X crystallization with novel (hierarchical) morphology from coal fly ash

机译:用新型(分层)形态从煤粉煤灰中对X沸石结晶进行原位超声诊断

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摘要

In this paper the applicability of an in situ ultrasonic diagnostic technique in understanding the formation process of zeolite X with a novel morphology was demonstrated. The complexity of the starting fly ash feedstock demands independent studies of the formation process for each type of zeolite since it is not known whether the crystallization mechanism will always follow the expected reaction pathway. The hierarchical zeolite X was noted to follow a solution phase-mediated crystallization mechanism which differs from earlier studies of the zeolite A formation process from unaged, clear solution extracted from fused fly ash. The use of the in situ ultrasonic monitoring system provided sufficient data points which enabled closer estimation of the time of transition from the nucleation to the crystal growth step. In order to evaluate the effect of temperature on the resulting in situ attenuation signal, synthesis at three higher temperatures (80, 90 and 94 ℃) was investigated. It was shown, by the shift of the US-attenuation signal, that faster crystallization occurred when higher temperatures were applied. The novel hierarchical zeolite X was comprised of intergrown disc-like platelets. It was further observed that there was preferential growth of the disc-shaped platelets of zeolite X crystals in one dimension as the synthesis temperature was increased, allowing tailoring of the hierarchical morphology.
机译:本文证明了原位超声诊断技术在理解具有新颖形态的X沸石形成过程中的适用性。起始粉煤灰原料的复杂性要求对每种类型的沸石的形成过程进行独立研究,因为尚不清楚结晶机理是否将始终遵循预期的反应路径。注意到分层沸石X遵循溶液相介导的结晶机理,该机理不同于早期对从熔融的粉煤灰中提取的未老化,澄清的溶液形成沸石A的研究。原位超声监测系统的使用提供了足够的数据点,从而可以更精确地估计从成核到晶体生长步骤的过渡时间。为了评估温度对产生的原位衰减信号的影响,研究了在三个较高温度(80、90和94℃)下的合成。通过US衰减信号的移动表明,当施加较高的温度时发生更快的结晶。新颖的分级沸石X由互生的盘状血小板组成。进一步观察到,随着合成温度的升高,沸石X晶体的盘状薄片在一维上优先生长,从而允许分级的形态。

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