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Surface reconstruction in TGS family crystals under humidity and temperature controls

机译:湿度和温度控制下THE族晶体的表面重建

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Surface reconstruction of TGS family single crystals has been investigated using AFM at ambient and controlled conditions. Domain boundary migration with simultaneous formation of holes at the boundary has been imaged for the first time. It is found that domain wall migration is accompanied by formation of elongat ed holes on originally negative end. Using humidity / temperature controlled AFM, holes on the positive end have been obtained with fast dehumidification while there is no such hole-formation with slow dehumidifica- tion. These observations provide direct evidences for a dissolution / recrystallization model accounting for hole / terrace formations. On the basis of this work, it is further proposed that the hole-formation upon the fast dehumidi- fication can be ascribed by mass transfer limitation (ki- netic control). On the contrary, with a slow dehumidifi- cation rate, the same crystal plane would resume a flatten termination to reduce the total surface energy (thermody- namic control).
机译:已经在环境和受控条件下使用原子力显微镜研究了TGS家族单晶的表面重建。第一次成像了在边界同时形成孔的区域边界迁移。发现畴壁迁移伴随着在原始负端上形成伸长的孔。使用湿度/温度控制的原子力显微镜,可以在快速除湿的情况下在正极上获得孔,而在缓慢除湿的情况下则不会形成孔。这些观察结果为解释孔/阶地层构造的溶解/再结晶模型提供了直接的证据。在这项工作的基础上,进一步提出,快速除湿时的孔形成可以归因于传质限制(动力学控制)。相反,在除湿速度较慢的情况下,同一晶面将恢复平坦的端接,以降低总表面能(热力学控制)。

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