Abstract
The grand canonical ensemble Monte Carlo method is used to simulate the behaviour of a marginally supercritical Lennard-Jones gas near a graphite surface. The results reproduce the cusp-like shape of the experimentally observed adsorption isotherms. Even at these high temperatures, the computations clearly show the occurrence of multilayer adsorption; up to four layers are discernible at sufficiently high pressures.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
