On the High-Temperature Phase Transition of GdSiGe.

The first-order monoclinic-to-orthorhombic (β→γ) phase transition of the giant magnetocaloric material GdSiGe was studied using in situ high-temperature single-crystal X-ray diffraction. A special crystal mounting procedure was developed to avoid crystal contamination by oxygen or nitrogen at high t...

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Publicado en:Journal of the American Chemical Society Vol. 127; no. 1; pp. 317 - 325
Autores principales: Mozharivskyj, Yurij, Pecharsky, Alexandra O., Pecharsky, Vitalij K., Miiler, Gordon J.
Formato: Artículo
Publicado: American Chemical Society 1/12/2005
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Acceso en línea:Ver este registro en EBSCOhost
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        atl: On the High-Temperature Phase Transition of GdSiGe.
      aug:
        au:
          Mozharivskyj, Yurij
          Pecharsky, Alexandra O.
          Pecharsky, Vitalij K.
          Miiler, Gordon J.
        affil:
          Ames Laboratory, Materials and Engineering Physics Program, Iowa State University, Ames, Iowa 50011-3020.
          Department of Materials Science and Engineering, Iowa State University, Ames, Iowa 50011-2300.
          Department of Chemistry, Iowa State University, Ames, Iowa 50011-3111.
      su:
        Physical & theoretical chemistry
        Oxygen
        Nitrogen
        Optical diffraction
        High temperatures
        Heat
      sug:
        subj:
          Physical & theoretical chemistry
          Oxygen
          Nitrogen
          Optical diffraction
          High temperatures
          Heat
      ab: The first-order monoclinic-to-orthorhombic (β→γ) phase transition of the giant magnetocaloric material GdSiGe was studied using in situ high-temperature single-crystal X-ray diffraction. A special crystal mounting procedure was developed to avoid crystal contamination by oxygen or nitrogen at high temperatures. The elastic β→γ transformation occurs at 300-320 °C during heating, and it is reversible during fast and slow heating and slow cooling but irreversible during rapid cooling. Contrary to theoretical predictions, the macroscopic distribution of the Si and Ge atoms remains the same in both the orthorhombic γ-polymorph and the monoclinic β-phase. It appears that interstitial impurities may affect stability of both the monoclinic and orthorhombic phases. In the presence of small amounts of air, the β→γ transformation is complete only at 600 °C. The interslab voids, which can accommodate impurity atoms, have been located in the structure, and an effect of partially filling these voids with oxygen or nitrogen atoms on the β→γ transition is discussed.
      pubtype: Academic Journal
      doctype: Article
      src: R
    language: English
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