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Pressure-induced crystallization of amorphous Ge_2Sb_2Te_5

机译:压力诱导非晶态Ge_2Sb_2Te_5的结晶

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摘要

Using in situ x-ray diffraction, we demonstrate a pressure-induced crystallization of as-deposited amorphous Ge_2Sb_2Te_5 (a-GST) into a body-centered-cubic (bcc) solid solution at 28 GPa, and the back transformation from the bcc-GST to a-GST. A large hysteresis loop was observed, as the bcc-GST was retained until 15 GPa. Comparisons have been made, employing the x-ray data and the structural information obtained from ab initio molecular dynamics simulations, between the as-deposited a-GST and the a-GST obtained from the pressure-induced collapse of the rocksalt GST, both at a high hydrostatic pressure (20 GPa) prior to their crystallization to bcc. The results suggest that both routes have resulted in the same high-pressure amorphous state, which explains their crystallization into bcc-GST at similar pressures.
机译:使用原位X射线衍射,我们证明了沉积后的非晶态Ge_2Sb_2Te_5(a-GST)在28 GPa压力下结晶为体心立方(bcc)固溶体,并从bcc- GST到a-GST。观察到较大的磁滞回线,因为bcc-GST一直保留到15 GPa。利用x射线数据和从头算分子动力学模拟获得的结构信息,对沉积的a-GST和由压力引起的岩盐GST塌陷获得的a-GST进行了比较,两者均在在结晶成密件抄送之前要承受较高的静水压力(20 GPa)。结果表明,这两种途径均导致相同的高压非晶态,这解释了它们在相似的压力下结晶为bcc-GST。

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  • 来源
    《Journal of Applied Physics》 |2010年第8期|p.083519.1-083519.5|共5页
  • 作者单位

    Department of Materials Science and Engineering, Johns Hopkins University, Baltimore, Maryland 21218, USA;

    rnHigh Pressure Collaborative Access Team, Carnegie Institution of Washington, Argonne, Illinois 60439, USA;

    rnDepartment of Materials Science and Engineering, Johns Hopkins University, Baltimore, Maryland 21218, USA;

    rnDepartment of Computational and Data Sciences, George Mason University, Fairfax, Virginia 22030, USA;

    rnInstitute of Microstructure and Property of Advanced Materials, Beijing University of Technology, Beijing 100124, People's Republic of China;

    rnDepartment of Materials Science and Engineering, Johns Hopkins University, Baltimore, Maryland 21218, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
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