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Structure Characterization of CuCl2-FeCl3-H2SO4 graphite intercalation compounds

机译:CuCl2-FeCl3-H2SO4石墨插层化合物的结构表征

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Graphite intercalation compounds (GIC) is important in both scientific research and technological application. GIC can be used as the precursors to fabricate new materials in correlation with carbon nanotubes (CNTs) or other CNTs associated nano-materials. In present work, graphite intercalation compounds with CuCl2-FeCl3-H2SO4 (GICs) have been synthesized via a hydrothermal treatment at 150 ℃ and exfoliation method. The structure and composition of these graphite intercalation compounds are analyzed by means of x-ray diffraction, energy dispersive x-ray (EDX microanalysis) and high-resolution transmission electron microscopy (HRTEM). The results demonstrate that the CuCl2-FeCl3-H2SO4 molecules have been successfully intercalated into the interlayer of graphite sheets. Temperature dependence of magnetization is measured from 5 K to 300 K. Two antiferromagnetic transitions of the graphite intercalation compounds are observed at low temperatures. The critical transition temperatures are estimated to be about 50 K and 102 K, respectively. The related magnetic properties are discussed briefly.
机译:石墨插层化合物(GIC)在科学研究和技术应用中都很重要。 GIC可用作制造与碳纳米管(CNT)或其他与CNT相关的纳米材料相关的新材料的前体。在目前的工作中,通过150℃水热处理和剥离法合成了具有CuCl2-FeCl3-H2SO4(GIC)的石墨插层化合物。通过x射线衍射,能量色散x射线(EDX显微分析)和高分辨率透射电子显微镜(HRTEM)分析了这些石墨插层化合物的结构和组成。结果表明,CuCl2-FeCl3-H2SO4分子已成功插入石墨片的夹层中。磁化强度的温度依赖性为5 K至300K。在低温下观察到石墨插层化合物的两个反铁磁跃迁。临界转变温度估计分别为约50 K和102K。简要讨论了相关的磁性能。

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