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Thermoelectricity Generation and Electron–Magnon Scattering in a Natural Chalcopyrite Mineral from a Deep‐Sea Hydrothermal Vent

Ran AngKey Laboratory of Radiation Physics and Technology, Ministry of Education, Institute of Nuclear Science and Technology, Sichuan University, Chengdu 610064 (China)Atta Ullah KhanNational Institute for Materials Science (NIMS), International Center for Materials Nanoarchitechtonics (MANA), Namiki 1-1, Tsukuba 305-0044 (Japan)Naohito TsujiiNational Institute for Materials Science (NIMS), International Center for Materials Nanoarchitechtonics (MANA), Namiki 1-1, Tsukuba 305-0044 (Japan)Ken TakaiDepartment of Subsurface Geobiological Analysis and Research (D-SUGAR) (Japan), Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka 273-0061 (Japan)Ryuhei NakamuraRIKEN Center for Sustainable Resource Science, Hirosawa 2-1, Wako, Saitama 351-0198 (Japan)Takao MoriNational Institute for Materials Science (NIMS), International Center for Materials Nanoarchitechtonics (MANA), Namiki 1-1, Tsukuba 305-0044 (Japan)
2015en
ABI

Аннотация

Abstract Current high‐performance thermoelectric materials require elaborate doping and synthesis procedures, particularly in regard to the artificial structure, and the underlying thermoelectric mechanisms are still poorly understood. Here, we report that a natural chalcopyrite mineral, Cu 1+x Fe 1−x S 2 , obtained from a deep‐sea hydrothermal vent can directly generate thermoelectricity. The resistivity displayed an excellent semiconducting character, and a large thermoelectric power and high power factor were found in the low x region. Notably, electron–magnon scattering and a large effective mass was detected in this region, thus suggesting that the strong coupling of doped carriers and antiferromagnetic spins resulted in the natural enhancement of thermoelectric properties during mineralization reactions. The present findings demonstrate the feasibility of thermoelectric energy generation and electron/hole carrier modulation with natural materials that are abundant in the Earth’s crust.

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