Abstract
The mass of chlorine gas or liquid adsorbed by graphite was measured with a recording silica spring balance designed to operate at pressures to saturation and sample temperatures to 25°C. The rates of absorption in saturated vapor and the isotherms were determined for several sources and flake sizes of graphite. All behaviour in the range −25° to +20°C was characteristic of condensation of chlorine in a pore system. Some of the behaviour was also characteristic of intercalation but the other behaviour was not. It is therefore concluded that chlorine does not intercalate graphite.
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