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The influence of crystallization conditions on the growth of polycrystalline particles of L-glutamic acid, an aromatic amine derivative and calcium carbonate

机译:结晶条件对L-谷氨酸,芳族胺衍生物和碳酸钙的多晶颗粒生长的影响

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The effect of initial supersaturation and temperature on the particle morphology of L-glutamic acid, an aromatic amine derivative and calcium carbonate was compared in batch experiments by reaction crystallization in water at temperatures of 5-90 deg C. It was found that both the aromatic amine and L-glutamic acid give rise to polycrystalline particles at higher initial supersaturation ratios. On the other hand, monocrystals were obtained at low values of the initial supersaturation, plate-like crystals in the aromatic amine system and needle-like particles of the beta-polymorph in the L-glutamic acid system. For the aragonite polymorph of calcium carbonate it has been observed that higher initial supersaturation ratios give rise to polycrystalline particles. This agrees well with the findings for the aromatic amine and L-glutamic acid which illustrates the role of the supersaturation in the switching from monocrystalline to polycrystalline growth. Moreover lower temperatures were found to favour polycrystalline growth of aragonite. Also for the calcite polymorph of calcium carbonate the switching from monocrystalline to polycrystalline growth was observed as the temperature was decreased. However, in this case the onset of polycrystalline growth might also be the effect of a higher level of supersaturation. Unlike aragonite and calcite, the normal enlargement mode of vaterite is polycrystalline growth. In the study of the vaterite polymorph the feed rate of Ca~(2+) was varied in seeded semi-batch experiments to study changes in the particle morphology. It was found that the crystal subunits are larger at an initial supersaturation ratio of S_(0)velence1.4 than at a higher value of S_(0)velence3 as a consequence of the higher degree of growth front nucleation at larger supersaturation.
机译:初始过饱和度和温度对L-谷氨酸的颗粒形态的影响,通过在水中的水中结晶在5-90℃的温度下进行分批实验进行比较。发现芳香族胺和L-谷氨酸以较高的初始过饱和比率产生多晶颗粒。另一方面,在初始过饱和的初始过饱和度的低值,在芳族胺系统中的板状晶体的低值下获得单晶,并在L-谷氨酸系统中的β-多晶型物的针状颗粒。对于碳酸钙的化石多晶型物,已经观察到较高的初始过饱和度量导致多晶粒颗粒。这与芳族胺和L-谷氨酸的发现吻合良好,其示出了过饱和在从单晶转换为多晶生长中的过饱和的作用。此外,发现较低的温度有利于化石的多晶生长。同样对于碳酸钙的方解石多晶型物,观察到从单晶到多晶生长的切换,因为温度降低。然而,在这种情况下,多晶生长的发作也可能是更高水平的过饱和度的效果。与金属石和方解石不同,Vaterite的正常增大模式是多晶生长。在Vaterite多晶型物的研究中,Ca〜(2+)的进料速率在种子半批量实验中变化,以研究颗粒形态的变化。结果发现,由于在较大的过饱和度下的更高程度的生长前成核,晶体亚基的初始超饱和度比S_(0)velence1.4的初始过饱和度较大。

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