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{100} -> {111} morphological change in KCl crystals grown from Pb2+-doped aqueous solutions

机译:从掺杂Pb2 +的水溶液中生长的KCl晶体中{100}-> {111}的形态变化

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摘要

KCl f.c.c. crystals generally exhibit a {100} habit when growing from pure aqueous solutions, a richer {100} + {111} morphology being obtained only under well-defined growth temperature and supersaturation. When increasing amounts (less than 2000 ppm) of Pb are put in a supersaturated solution, the KCl growth morphology undergoes a progressive change: {100} -> {100} + {111} -> {111}. Detailed growth patterns have been investigated by means of SEM and AFM, while EDS and XRF analyses allowed us to ascertain that Pb is not only adsorbed on the growing KCl surfaces but also selectively absorbed within the {111} growth sectors. Starting from recent and analogous findings, we tried to interpret the morphological change by means of a geometric and structural model of epitaxy between the {100} and the {111} forms of KCl and the most important forms of those compounds that could be adsorbed on them: PbCl2 (cotunnite), PbCl(OH) (laurionite-paralaurionite) and KCl.PbCl2 (challacolloite). Excellent lattice coincidences have been found, thus proving that the {111} KCl octahedron is largely privileged for adsorption/absorption to occur with respect to the {100} KCl cube. Based on this ground, simple kinetic considerations can be proposed to satisfactorily explain the observed morphology change.
机译:氯化钾从纯水溶液中生长时,晶体通常表现出{100}习惯,只有在明确定义的生长温度和过饱和条件下,才能获得更丰富的{100} + {111}形态。当将过量(小于2000 ppm)的Pb放入过饱和溶液中时,KCl的生长形态会逐渐变化:{100}-> {100} + {111}-> {111}。详细的生长方式已通过SEM和AFM进行了研究,而EDS和XRF分析使我们可以确定Pb不仅吸附在生长的KCl表面上,而且还选择性地吸附在{111}生长区内。从最近的类似发现开始,我们试图通过{100}和{111}形式的KCl与最重要形式的那些可能被吸附的化合物之间的外延的几何和结构模型来解释形态变化。它们是:PbCl2(共辉石),PbCl(OH)(月桂石-次月桂石)和KCl.PbCl2(硅铝石)。已经发现极好的晶格重合,因此证明{111} KCl八面体在相对于{100} KCl立方体的吸附/吸收方面具有很大的特权。在此基础上,可以提出简单的动力学考虑因素,以令人满意地解释观察到的形态变化。

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