論文 Observation of current whirlpools in graphene at room temperature

Marius L. Palm ; Chaoxin Ding ; William S. Huxter ; Takashi Taniguchi SAMURAI ORCID (National Institute for Materials Science) ; Kenji Watanabe SAMURAI ORCID (National Institute for Materials Science) ; Christian L. Degen

コレクション

引用
Marius L. Palm, Chaoxin Ding, William S. Huxter, Takashi Taniguchi, Kenji Watanabe, Christian L. Degen. Observation of current whirlpools in graphene at room temperature. Science. 2024, 384 (6694), 465-469. https://doi.org/10.1126/science.adj2167

説明:

(abstract)

Electron-electron interactions in high-mobility conductors can give rise to transport signatures resembling those described by classical hydrodynamics. Using a nanoscale scanning magnetometer, we image a striking hydrodynamic transport patern – stationary current vortices – in a monolayer graphene device at room temperature. By measuring devices with increasing characteristic size, we observe the disappearance of the current vortex and thus verify a prediction of the hydrodynamic model. We further observe that vortex flow is present for both hole- and electron-dominated transport regimes, but disappears in the ambipolar regime. We atribute this effect to a reduction of the vorticity diffusion length near charge neutrality. Our work showcases the power of local imaging techniques for unveiling exotic mesoscopic transport phenomena.

権利情報:

  • In Copyright
    This is the author’s version of the work. It is posted here by permission of the AAAS for personal use, not for redistribution. The definitive version was published in Science on Volume 384, 25 Apr 2024, DOI:10.1126/science.adj2167.

キーワード: hydrodynamic transport, current vortex, graphene device

刊行年月日: 2024-04-26

出版者: American Association for the Advancement of Science (AAAS)

掲載誌:

  • Science (ISSN: 10959203) vol. 384 issue. 6694 p. 465-469

研究助成金:

原稿種別: 著者最終稿 (Accepted manuscript)

MDR DOI:

公開URL: https://doi.org/10.1126/science.adj2167

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更新時刻: 2025-07-23 16:30:35 +0900

MDRでの公開時刻: 2025-07-23 16:20:22 +0900

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