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在石墨层上合成和表征硫化钒的方钠石形式。

Synthesis and characterization of patronite form of vanadium sulfide on graphitic layer.

机构信息

Interdisciplinary School of Green Energy, Low Dimensional Carbon Materials Center and UNIST Central Research Facilities, UNIST (Ulsan National Institute of Science and Technology), UNIST-gil 50, Ulsan 689-798, Republic of Korea.

出版信息

J Am Chem Soc. 2013 Jun 12;135(23):8720-5. doi: 10.1021/ja403232d. Epub 2013 May 29.

Abstract

With the exploding interest in transition metal chalcogenides, sulfide minerals containing the dianion S2(2-), such as pyrite (FeS2), cattierite (CoS2), and vaesite (NiS2), have recently attracted much attention for potential applications in energy conversion and storage devices. However, the synthesis of the patronite structure (VS4, V(4+)(S2(2-))2) and its applications have not yet been clearly demonstrated because of experimental difficulties and the existence of nonstoichiometric phases. Herein, we report the synthesis of VS4 using a simple, facile hydrothermal method with a graphene oxide (GO) template and the characterization of the resulting material. Tests of various templates such as CNT, pyrene, perylene-3,4,9,10-tetracarboxylic dianhydride (PTCDA), and graphite led us to the conclusion that the graphitic layer plays a role in the nucleation during growth of VS4. Furthermore, the VS4/rGO hybrid was proved to be a promising functional material in energy storage devices.

摘要

随着对过渡金属硫属化物的兴趣不断增加,含有二负离子 S2(2-)的硫化物矿物,如黄铁矿 (FeS2)、钴硫矿 (CoS2) 和镍硫矿 (NiS2),最近因其在能源转换和存储设备中的潜在应用而受到广泛关注。然而,由于实验困难和存在非化学计量相,patronite 结构 (VS4,V(4+)(S2(2-))2) 的合成及其应用尚未得到明确证明。在此,我们使用简单、方便的水热法,以氧化石墨烯 (GO) 模板合成了 VS4,并对所得材料进行了表征。对各种模板(如 CNT、芘、苝-3,4,9,10-四羧酸二酐 (PTCDA) 和石墨)的测试使我们得出结论,在 VS4 的生长过程中,石墨层在成核中起作用。此外,VS4/rGO 杂化物被证明是一种有前途的储能设备中的功能材料。

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