When the bromine residue in graphite is heated and cooled between 20" and 900ยฐC there is an emission of Brz over certain relatively small temperature ranges on both heating and cooling. It is shown that two of these emissions are associated with observed decreases in X-ray diffraction spacing betwee
Ellipsometric investigation of the intercalation threshold in the graphite and bromine system
โ Scribed by J.D. Hibbs; D.A. Young
- Publisher
- Elsevier Science
- Year
- 1978
- Tongue
- English
- Weight
- 514 KB
- Volume
- 53
- Category
- Article
- ISSN
- 0009-2614
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โฆ Synopsis
T&e adsorption of bromine onto the basal (0001) surface of highly oriented pyrolytic pphite is studied as a function of pressure at 25ยฐC by au ellipsometric technique. Below the intercalation threshold, the extend of adsorption is given direct!y by-variations in P, in tan ti e.up(iA) = rp/rs, svhi!e I& remains constant. At the threshold (20 torr Brz) $ falk steeply because ihtercalation here causes a discontinuous change in the substrate optical constants R and k. Reasons are given for supposing
๐ SIMILAR VOLUMES
Vapor pressure-composition diagram of the graphite-bromine system shows continuous changes in composition between the definite stages. It also shows a large hysteresis in the process of bromination-debromination. X-ray studies show that an intermediate compound at a composition between definite stag
## Abstractlntercalation of bromine at 20ยฐC into spectroscopic grade SP-I natural graphite flakes oxidized previously to four levels of burn-off has been studied. The threshold pressure, equilibrium amounts taken up at relative pressures up to 0.95, and the diffusion coefficient for bromine uptake
In the system FeCl,/Cl,/graphite, threshold values exist both for the vapor pressure of the halide and for the chlorine pressure. If the pressures are lower than required by the law of mass action, (pressures in mbar), the intercalation is blocked. The equilibrium is attributed to the nucleation p
Electrical conductivity, transverse magnetoresistance, and Hall coefficient, both of graphite in the course of bromination and of potassium-graphite intercalation compounds (K-GICs) in the course of ammoniation, were determined. Concentrations and mobilities of holes and electrons (q,, it,, p+, kc)