2 research outputs found
Structural single and multiple molecular adsorption of CO2 and H2O in zeolitic imidazolate framework (ZIF) crystals
No full text9 pags.; 5 figs.; 4 tabs.© 2015 Elsevier Inc. Abstract Theoretical methods are used for modelling the capture and storage of CO2 in Zinc-Imidazolate-Frameworks (ZIFs). Density functional theory (DFT) is employed to establish the structure of three ZIFs with small, medium and large cages to predict the uptake behaviour of adsorbed water and carbon dioxide. Water hydration strength and configuration inside the material are investigated with and without the presence of CO2. CO2 is predominantly located around the inner surface of the cages in the ZIFs type ZIFn (n = 1,4,6) through single and multipoint interactions. Water shows a stronger adsorption than carbon dioxide and can play an important role in solvating the CO2 molecules inside the porous. In the final structures, H2O and CO2 do not react with the surface to produce hydroxyl groups or carbonate-like species, respectively. Both species compete for the same adsorption sites. Their maximum adsorption occurs in systems with really accessible surfaces such us ZIF6. A detailed study of the surface-accessibility of a molecule on a >Connolly Surface> is reported, were ZIFs with extra-large pores plays a major role on the adsorption process. Simulated adsorption isotherms throughout MC simulations were obtained for a single CO2 and H2O in which results give a ranking for the most appropriate process conditions.This research was supported by a Marie Curie International
Research Staff Exchange Scheme Fellowship within the 7th European
Community Framework Program under Grant No. PIRSES-GA-
2012-31754, the COST ACTIONS 1401 and 1405 and the MINECO of
Spain grant FIS2013-40626-P. Supercomputer time by the CTI-CSIC
and CESGA centers are also acknowledged. This work has benefited
from a French government grant managed by ANR within the frame
of the national program investments for the future ANR-11-LABX-
022-01.Peer Reviewe
