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The separate roles of shear rate and mixing on gibbsite precipitation

机译:剪切速率和混合对三水铝石沉淀的独立作用

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摘要

Methods are presented for quantifying the shear rate and mixing during laboratory precipitation. These are used to investigate the separate effects of shear rate and mixing on gibbsite precipitation from caustic aluminate solutions. Experiments were performed under conditions where the "chemistry" (i.e. the liquor composition, temperature and seed) and the shear rates were the same but the "mixing" was different. Precipitation experiments were conducted in both the laminar and turbulent flow regimes. The laminar flow regime experiments were performed in a Taylor-Couette precipitator, whereas the turbulent regime experiments were performed in a stirred tank. It was observed that in a high-shear, turbulent, well-mixed, stirred precipitator the effect of mixing on the product CSD is negligible compared to the effect of mean shear rate. This suggests that, unlike many precipitation systems for which the kinetics estimates are affected by micromixing effects, it should be possible to estimate the underlying gibbsite kinetics, at least in high-shear stirred tank experiments. The turbulent and laminar flow regime experiments both suggest that mixing does not significantly affect the desupersaturation kinetics.
机译:提出了量化实验室沉淀过程中剪切速率和混合的方法。这些用于研究剪切速率和混合对苛性铝酸盐溶液中菱铁矿沉淀的单独影响。实验是在“化学”(即液体组成,温度和种子)和剪切速率相同但“混合”不同的条件下进行的。在层流和湍流状态下都进行了沉淀实验。层流状态实验是在Taylor-Couette除尘器中进行的,而湍流状态实验是在搅拌釜中进行的。观察到在高剪切,湍流,充分混合,搅拌的沉淀器中,与平均剪切速率的影响相比,混合对产物CSD的影响可忽略不计。这表明,与许多动力学估算受微混合效应影响的降水系统不同,至少在高剪切搅拌釜实验中,应该有可能估算潜在的三水铝石动力学。湍流和层流状态实验均表明混合不会显着影响去饱和动力学。

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