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C-axis resistance of HgCl2 intercalated graphite as a function of temperature and pressure

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Authors

  • O. E. Andersson
  • P. Behrens
  • B. Sundqvist

External Research Organisations

  • Umea University
  • Universität Hamburg
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Details

Original languageEnglish
Pages (from-to)485-490
Number of pages6
JournalSynthetic metals
Volume34
Issue number1-3
Publication statusPublished - 1989
Externally publishedYes

Abstract

The c-axis resistance of stage 3 HgCl2 intercalated graphite has been measured as a function of temperature T and pressure p in the range 40 to 300 K and up to 1 GPa (10 kbar). The absolute resistivity and its T- and p- dependence are all in good agreement with data for other acceptor compounds. The measurements show that a previosly unknown phase transformation occurs above 0.4 GPa. Below 250 K the high pressure phase is metastable down to zero pressure, and an x-ray diffraction analysis of metastable material shows that no stage change occurs. The transition thus probably leads to a different in-plane structure characterized by a more densely packed intercalate layer.

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Cite this

C-axis resistance of HgCl2 intercalated graphite as a function of temperature and pressure. / Andersson, O. E.; Behrens, P.; Sundqvist, B.
In: Synthetic metals, Vol. 34, No. 1-3, 1989, p. 485-490.

Research output: Contribution to journalArticleResearchpeer review

Andersson OE, Behrens P, Sundqvist B. C-axis resistance of HgCl2 intercalated graphite as a function of temperature and pressure. Synthetic metals. 1989;34(1-3):485-490. doi: 10.1016/0379-6779(89)90429-3
Andersson, O. E. ; Behrens, P. ; Sundqvist, B. / C-axis resistance of HgCl2 intercalated graphite as a function of temperature and pressure. In: Synthetic metals. 1989 ; Vol. 34, No. 1-3. pp. 485-490.
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abstract = "The c-axis resistance of stage 3 HgCl2 intercalated graphite has been measured as a function of temperature T and pressure p in the range 40 to 300 K and up to 1 GPa (10 kbar). The absolute resistivity and its T- and p- dependence are all in good agreement with data for other acceptor compounds. The measurements show that a previosly unknown phase transformation occurs above 0.4 GPa. Below 250 K the high pressure phase is metastable down to zero pressure, and an x-ray diffraction analysis of metastable material shows that no stage change occurs. The transition thus probably leads to a different in-plane structure characterized by a more densely packed intercalate layer.",
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AU - Andersson, O. E.

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AU - Sundqvist, B.

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