X-ray determination of the modulation potential in a stage-2 potassium-graphite intercalation compound

1989 ◽  
Vol 39 (15) ◽  
pp. 10627-10632 ◽  
Author(s):  
X. B. Kan ◽  
J. L. Robertson ◽  
S. C. Moss ◽  
K. Ohshima ◽  
C. J. Sparks
Carbon ◽  
1995 ◽  
Vol 33 (2) ◽  
pp. 177-181 ◽  
Author(s):  
V.A. Nalimova ◽  
D. Guérard ◽  
M. Lelaurain ◽  
O.V. Fateev

1995 ◽  
Vol 10 (5) ◽  
pp. 1196-1199 ◽  
Author(s):  
Takeshi Abe ◽  
Yasuo Mizutani ◽  
Mitsuru Asano ◽  
Toshio Harada

Intercalation of AlCl3 into stage 2 FeCl3-graphite intercalation compound (GIC) using an ordinary two-bulb method has been studied by x-ray diffraction. Stages 2, 3, and 4 ternary AlCl3-FeCl3-GlC's are obtained when the temperatures of the stage 2 FeCl3-GIC were set at T (GIC) = 503, 523, and 553 K, respectively, for the AlCl3 intercalate material at T (AlCl3) = 473 K, that is, the vapor pressure of (AlCl3)2 (g) of the main vapor species to be held at p {(AlCl3)2} = 2.4 × 105 Pa. However, for the temperature of the stage 2 FeCl3-GIC at T (GIC) = 573 K, the (AlCl3)2 (g) vapor is found to promote the decomposition of the stage 2 FeCl3-GIC, resulting in the formation of graphite. The decomposition of the stage 2 FeCl3-GIC is considered to take place because the complex AlFeCl6 (g) in the gas phase, which is formed from both (AlCl3)2 (g) and FeCl3 existing at the edge of the FeCl3-GIC, is thermodynamically more stable than the FeCl3 and AlCl3 intercalates in their GIC at p {(AlCl3)2} = 2.4 × 105 Pa and T (GIC) = 573 K.


2014 ◽  
Vol 552 ◽  
pp. 328-330
Author(s):  
Zhi Guo Liu

In order to investigate the structural evolution of natural flake graphite during intercalation and exfoliation, natural graphite flakes were treated by intercalating, water-washing, drying and expanding. The corresponding products, graphite intercalation compound (GIC), residue GIC (expandable graphite) and expanded graphite were characterized by X-ray diffraction (XRD). The results can provide reference for the research in this field.


2002 ◽  
Vol 17 (12) ◽  
pp. 3190-3192 ◽  
Author(s):  
H. Shioyama ◽  
M. B. H. M. Saman ◽  
A. Sanpanich

Intercalation of EuCl3 TbCl3, and AlCl3 into graphite was carried out in the presence of chlorine. The observation of products by x-ray diffraction showed that the extent of chloride intercalation could be controlled through adjustment of the pressure of chlorine; increasing pressure tended to increase the extent of intercalation. In the case of EuCl3, the extent of intercalation varied to show a stage transition. In contrast, TbCl3 intercalation gave a mixture of stage 2 or stage 4 graphite intercalation compound (GIC) and remaining graphite, where the extent of intercalation is revealed by the ratio of GIC to graphite. With respect to AlCl3 intercalation, although the preparation of stage 1, 2, and 4 GICs was successful, stage 3 and 5 GICs could not be obtained.


1995 ◽  
Vol 75 (5) ◽  
pp. 942-945 ◽  
Author(s):  
David G. Wiesler ◽  
Masatsugu Suzuki ◽  
Itsuko S. Suzuki ◽  
Nicholas Rosov

2021 ◽  
Vol 26 (2) ◽  
Author(s):  
José Armando Espinosa Martinez ◽  
Miguel Sanchez Junior ◽  
Augusto Nobre Golçalves ◽  
Roxana Maria Martinez Orrego ◽  
Odila Florêncio

ABSTRACT Three different processes for the synthetization of exfoliated graphite intercalation compound have been tested in two different type of graphite, one in powder form and the other one as flakes. Each graphite was oxidized applying the same experimental conditions (sonification, neutralization, filtering and drying) but using three different auxiliary oxidizers (H2O2, HNO3 and KClO3) previously mixed with H2SO4. The resulting synthesized samples were characterized by X-ray diffraction, Raman spectroscopy and scanning electron microscopy. The Raman spectra analysis of the oxidized samples correspond to that of a graphene of few layers. Stronger delamination and exfoliation were observed in the samples of graphite, originally in powder form, treated with H2SO4/HNO3.


1996 ◽  
Vol 11 (12) ◽  
pp. 3039-3044 ◽  
Author(s):  
Takeshi Abe ◽  
Yasukazu Yokota ◽  
Yasuo Mizutani ◽  
Mitsuru Asano ◽  
Toshio Harada ◽  
...  

X-ray diffraction (XRD) and Raman spectroscopy have been used for the study of the bi-intercalation of SbCl5 into a stage 5 FeCl3-graphite intercalation compound (GIC). The stage 5 FeCl3-GIC is prepared by an ordinary two-bulb method with the temperature of graphite at 788 K and that of FeCl3 at 573 K. The FeCl3-SbCl5-graphite bi-intercalation compound (GBC) with one SbCl5 layer is obtained when the temperature of the stage 5 FeCl3-GIC is held at 443 K and the temperature of SbCl5 at 373 K in the two-zone system. The stacking sequence of the GBC is found to be an admixture of G(FeCl3)GG(SbCl5)GGG(FeCl3)G and G(FeCl3)GGG(SbCl5)GG(FeCl3)G by XRD, where G, (FeCl3), and (SbCl5) are the graphite, FeCl3, and SbCl5 layers, respectively. The Raman spectrum of the GBC shows two peaks associated with the and modes at 1588 cm−1 and 1610 cm−1, respectively. For the temperatures of stage 5 FeCl3-GIC at 443 K and SbCl5 at 403 K in the two-zone system, the FeCl3-SbCl5-GBC with two SbCl5 layers is obtained. The stacking sequence of the GBC is determined to be an admixture of G(FeCl3)GG(SbCl5)GG(SbCl5)G(FeCl3)G and G(FeCl3)G(SbCl5)GG(SbCl5)GG(FeCl3)G In the Raman spectrum of this GBC, two peaks associated with the mode are observed at 1616 and 1624 cm−1.


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