Einaga Mari, Sakata Masafumi, Ishikawa Takahiro, Shimizu Katsuya, Eremets Mikhail I, Drozdov Alexander P, Troyan Ivan A, Hirao Naohisa, Ohishi Yasuo
KYOKUGEN, Graduate School of Engineering Science, Osaka university, Machikaneyamacho 1-3, Toyonaka, Osaka, 560-8531, Japan.
Max-Planck Institut für Chemie, Hahn-Meitner-Weg 1, 55128 Mainz, Germany.
Nat Phys. 2016 Sep;12(9):835-838. doi: 10.1038/nphys3760. Epub 2016 May 9.
A superconducting critical temperature above 200 K has recently been discovered in HS (or DS) under high hydrostatic pressure1, 2. These measurements were interpreted in terms of a decomposition of these materials into elemental sulfur and a hydrogen-rich hydride that is responsible for the superconductivity, although direct experimental evidence for this mechanism has so far been lacking. Here we report the crystal structure of the superconducting phase of hydrogen sulfide (and deuterium sulfide) in the normal and superconducting states obtained by means of synchrotron X-ray diffraction measurements, combined with electrical resistance measurements at both room and low temperatures. We find that the superconducting phase is mostly in good agreement with theoretically predicted body-centered cubic (bcc) structure for HS (Ref.3). The presence of elemental sulfur is also manifest in the X-ray diffraction patterns, thus proving the decomposition mechanism of HS to HS + S under pressure4-6.
最近发现,在高静水压力下,硫化氢(或重硫化氢)的超导临界温度高于200K 。这些测量结果被解释为这些材料分解为元素硫和一种负责超导性的富氢氢化物,尽管到目前为止还缺乏这种机制的直接实验证据。在这里,我们报告了通过同步加速器X射线衍射测量获得的硫化氢(和硫化氘)超导相在正常态和超导态下的晶体结构,并结合了室温和低温下的电阻测量。我们发现,超导相与理论预测的硫化氢体心立方(bcc)结构基本一致(参考文献3)。元素硫的存在也在X射线衍射图谱中得到体现,从而证明了硫化氢在压力下分解为硫化氢 + 硫的机制。