流动驱动的稀土硅酸盐管的传输限制生长

IF 3.1 Q2 CHEMISTRY, MULTIDISCIPLINARY ChemSystemsChem Pub Date : 2024-09-04 DOI:10.1002/syst.202400053
Panna E. Farkas, Emese Lantos, Dezső Horváth, Agota Tóth
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引用次数: 0

摘要

将稀土金属盐溶液注入硅酸钠溶液会产生垂直生长的管状沉淀结构。在输入浓度较低时,反应动力学为速率-去除过程,导致线性生长速率与注入速率无关。在较高浓度下,流动驱动沉淀生长,其特点是喷射机制。在所研究的稀土金属硅酸盐中,硅酸镝的结构最为坚硬,即使在较高的注入率下也能看到明显的增长。空心管的外表面是光滑的,根据能量色散 X 射线光谱测量结果,稀土氢氧化物在其上聚集成球状。
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Transport-Limited Growth of Flow-Driven Rare-Earth Silicate Tubes

The injection of rare-earth metal salt solutions into sodium silicate solution results in vertically growing tubular precipitate structures. At low input concentrations reaction kinetics is the rate-detemining process, leading to linear growth rates independent of injection rates. At higher concentrations, flow drives the precipitate growth, characterized by jetting mechanism. Among the studied rare-earth metal silicates, dysprosium silicate is found to have the most rigid structure with visible growth even at higher injection rates. The outer surface of the hollow tubes is smooth, on which rare-earth hydroxide – based on the result of the energy dispersive X-ray spectroscopy measurements – aggregates into globules.

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