天然和合成磷灰石单晶形态个性的热力学解释

Takaomi Suzuki, Haruka Takemae, Mika Yoshida
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引用次数: 2

摘要

利用水与甲酰胺液滴的接触角与晶面生长长度(h)对比,测定了同一母岩中天然氟磷灰石钙和同一原料合成的氯磷灰石钡的比表面自由能(SSFE)。不同晶体在相同的指标面下,实验得到的SSFE值也不同。SSFEs在晶体的各个面也有广泛的分布。我们认为观测到的地表应力强度不仅是理想平坦地台面的地表应力强度,而且还包括了地表应力自由能的贡献。虽然我们实验得到的晶体是生长形式,但SSFE与h之间的关系几乎是成正比的,这看起来像是在定性地满足Wulff关系。SSFE与h线的斜率反映了晶体生长的驱动力,较大晶体的曲线斜率较小。晶体越大,晶体生长的驱动力越小,这也意味着晶体越大,化学势越大。同一批次的晶体的个性可以用每个晶体的化学势的不同来解释。
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Thermodinamic Interpretaion of the Morphology Individuality of Natural and Synthesized Apatite Single Crystals
Specific surface free energy (SSFE) of natural calcium fluorapatite from the same mother rock and synthesized barium chlorapatite from the same lot was determined using contact angle of water and formamide droplets, compared with grown length of crystal face (h). The experimentally obtained SSFEs have different values even for the same index faces of the different crystals. The SSFEs also have wide distribution for each face of crystals. Observed SSFE is considered to be not only the SSFE of ideally flat terrace face, but also includes the contribution of strep free energy. Though the crystals we experimentally obtained were growth form, the relationship between SSFE and h was almost proportional, which looks like satisfying Wulff’s relationship qualitatively. The slope of SSFE versus h line shows the driving force of crystal growth, and the line for larger crystal has less steep slope. The driving force of crystal growth for larger crystal is smaller, which also means that the chemical potential is larger for larger crystal. The individuality of crystals for the same lot can be explained by the difference of the chemical potential of each crystal.
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