Abstract

Observation of ferromagnetic and granular superconductive features in highly-oriented-pyrolytic-graphite (HOPG) has recently attracted an important attention. We report a novel temperature dependent XRD and SQUID investigation of HOPG in the temperature range from 300.15 to 77.15 K. Unusual hysteresis features indicate the possible presence of vortex states in conditions of magnetic field approximately perpendicular to the HOPG layers. This interpretation is further supported by additional measurements performed on intermediate lamellae extracted by exfoliation. Evidence of a possible structural-transition in the c-axis of HOPG in the temperature range between 77 K and 100K is also provided by using the Rietveld refinement method. ZFC and FC measurements performed at high field values of 5000–10000 Oe, together with mFC-mZFC subtraction, highlight absence of a sharp depletion of the difference between magnetization signals towards zero. These observations may indicate the possible presence of additional unsaturated weak features, which are ascribed to superconductive signals as previously predicted by Scheike et al (Scheike et al 2013 Carbon; 59:140).

Highlights

  • Introduction cri ptUnderstanding the origin of magnetic ordering in pure carbon-based graphitic materials has recently become a crucial focus of research towards translation of these systems into technological applications

  • The layered structure of the highly oriented pyrolytic graphite (HOPG) sample was firstly revealed by XRD measurements, as indicated in Fig.1, with the observation of preferred 002 and 004 reflections

  • Instead by extracting the c-axis shift in pte the temperature range from 300 to 77K with Rietveld refinement, our results show a much weaker value of c-axis shift, namely -0.0008 nm

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Summary

Citation for published version

Ayoub and Xia, JiaChen and Guo, Jian and Shuai, Gao and Odunmbaku, Omololu and. Min and Shang, Hongyan and Corrias, Anna and Boi, Filippo (2020) Magnetic vortex and unsaturated magnetization components in highly oriented pyrolytic graphite.

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Results and Discussion cri pt
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