In silico screening of zeolites for application in high pressure hydrogen dehydration

Master thesis (2020)

Authors

D.F. Geerdink Applied Sciences

Contributors

T.J.H. Vlugt Engineering Thermodynamics - Mechanical, Maritime and Materials Engineering (mentor)
E.A. Pidko ChemE/Inorganic Systems Engineering - AS (graduation committee member)
O. Moultos Engineering Thermodynamics - Mechanical, Maritime and Materials Engineering (coach)
M. Erdös Engineering Thermodynamics - Mechanical, Maritime and Materials Engineering (coach)
Faculty
Applied Sciences, Applied Sciences
Copyright: © 2020 Daan Geerdink
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Published Date

17-04-2020

Language

English

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Faculty

Applied Sciences

Abstract

The energy mix of the future is likely to feature hydrogen due to its versatility. For effective use in energy storage, hydrogen has to be compressed. Conventional electrolysis of water and subsequent mechanical compression of hydrogen is an energy intensive process. A one-step conversion and compression can take place in a Electrochemical Hydrogen Compressor (EHC). This has the disadvantage that the resulting stream of high pressure hydrogen contains water. In order to assess the capability of hydrophilic zeolites as a means of selectively adsorbing this water, a in silico screening study of 6 zeolites was performed. To this end, a force field was constructed to allow for the simulation of high pressure hydrogen dehydration using Monte Carlo methods. The validity of this force field was evaluated by replicating simulation studies of adsorption of water/ hydrogen on zeolite frameworks with the presence of extra-framework cations. At the system pressure of 875 bar, prediction of the fugacity coefficient by means of the Peng-Robinson Equation of State (PR-EOS) yields inaccurate results. Therefore, these are calculated in the CFCNPT ensemble. It is demonstrated that the Ideal Adsorbed Solution Theory (IAST) is not suited to predict binary adsorption isotherms in this system. As a result of the screening study, it is found that the selectivity of water over hydrogen is almost linearly correlated to the amount of Al atoms in the zeolite framework. Furthermore, it is observed that topologies which feature a low amount of void space outperform those where significant void spaces are present. This can be attributed to the fact that the interactions of the zeolite with water are stronger than those with hydrogen in the limit of a low Si/Al ratio (Si/Al=1). It is theorized that water adsorbs preferentially at the surface of the zeolite, and competitive adsorption by hydrogen can only take place in sufficiently large void spaces.