Published December 10, 2009 | Version v1
Journal article

Equilibrium conversion in Cu-Cl cycle multiphase processes of hydrogen production

  • 1. Faculty of Engineering and Applied Science, University of Ontario Institute of Technology, 2000 Simcoe Street North, Oshawa, L1H 7K4 Ontario (Canada)

Description

This paper performs a thermodynamic equilibrium analysis of individual steps within the copper-chlorine (Cu-Cl) thermochemical cycle of hydrogen production. The cycle has a maximum temperature of 550 oC and it involves four reaction steps - producing hydrogen, copper, hydrogen chloride and oxygen - and a cupric chloride drying step. In this paper, the chemical reaction steps of the cycle are analyzed to determine the effects of process variables on chemical equilibrium conversion. It is found that the hydrogen production reaction can occur as a two-phase gas-solid system, rather than three phases. The optimal conditions for hydrogen production occur at a temperature below 400 oC, at atmospheric pressure. The study also found that the ideal condition to minimize excess steam, and completely consume any chlorine formed during the reaction, is a temperature of 400 oC, at atmospheric pressure. The operating conditions for complete consumption of chlorine were identified by the equilibrium partial pressure of chlorine formed, during decomposition of cupric chloride solid (CuCl2), and the equilibrium partial pressure of chlorine from the reverse chlorine consumption reaction. Furthermore, the ideal condition for the copper oxychloride decomposition reaction is a temperature around 500 oC, atmospheric pressure, which minimizes cuprous chloride (CuCl) vaporization.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.tca.2009.07.009

Additional details

Identifiers

DOI
10.1016/j.tca.2009.07.009;
PII
S0040-6031(09)00295-0;

Publishing Information

Journal Title
Thermochimica Acta
Journal Volume
496
Journal Issue
1-2
Journal Page Range
p. 117-123
ISSN
0040-6031
CODEN
THACAS

Optional Information

Copyright
Copyright (c) 2009 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.