Modelling of the kinetics of sulphation of CaO particles under CaL reactor conditions. (15th June 2015)

• Record Type: Journal Article
• Authors: Cordero, J.M.; Alonso, M.
• Is Part Of: Fuel. Volume 150(2015)
• Page Start: 501
• Page End: 511
• Publication Date: 2015-06-15
• Subjects: Sulphation kinetics -- SO2 capture -- Calcium looping -- CO2 capture -- RPM -- CFB; Fuel -- Periodicals; Coal -- Periodicals; Coal; Fuel; Periodicals; 662.6
• DOI: 10.1016/j.fuel.2015.02.075
• Languages: English
• ISSNs: 0016-2361

Abstract

Highlights: The CaL CFB reactors were found to be excellent desulphurization systems. The purge from the calciner proved to be a better SO2 sorbent than fresh limestone. The RPM applied was suitable for predicting the sulphation conversions under CaL conditions. Abstract: CO2 capture in a calcium looping (CaL) system is one of the most promising technologies for climate change mitigation. The main reactors in these systems (carbonator and calciner) operate in conditions where the reaction of CaO with the SO2 resulting from the combustion of coal is inevitable. This work reports on the sulphation of CaO under a range of variables that are typical of reactors in CaL systems. Furthermore it is demonstrated that the number of calcination carbonation cycles changes the sulphation patterns of the CaO from heterogeneous to homogeneous in all the limestones tested. For 50 carbonation calcination cycles and for particle sizes below 200 μm, the sulphation pattern is in all cases homogeneous. The sulphation rates were found to be first order with respect to SO2, and zero with respect to CO2 . Steam was observed to have a positive effect only in the diffusion through the product layer controlled regime, as it leads to an improvement in the sulphation rates and effectiveness of the sorbent. Most of the experimental results of sulphation of highly cycled sorbents under all conditions can be fitted by means of the Random Pore Model (RPM) assuming that the kinetics and diffusion through the product layer of the CaSO4 are the controlling regimes.