Reports: AC3

47641-AC3 Ion Exchange of Zeolites in Polyethylene Oxide Oligomer Solutions

Susan E. Latturner, Florida State University

Poly(ethylene oxide) oligomers, commonly referred to as polyethylene glycols or PEGs, are polyethers that are liquid at room temperature and have high enough melting points to enable their use as ion exchange media at elevated temperatures.  We have found PEG oligomers to be effective as alternative solvents for the ion-exchange of porous and layered oxide materials.  Our initial work explored lithium ion exchange into sodalite, using PEGs of varying molecular weight and end-capping groups. Based on the successful results of these experiments, exchange of catalytically active ions Mn2+, Fe2+, and Co2+ into hydrated and dehydrated Zeolite X (Na80Al80Si112O384·nH2O) in PEG solvents was explored.  When attempted in aqueous solutions, exchange of these cations quickly leads to destruction of the zeolite structure within 1 – 2 exchange cycles.  However, in PEG oligomer solvents, the structure can be maintained and exchanges of 48% (Co2+), 80% (Mn2+), and 91% (Fe2+) are observed after one cycle under hydrated conditions.  When rigorous steps are taken to remove all water from the zeolite before exchange, absorption of the oligomers into the zeolite pores is promoted which hinders ion exchange; a maximum of 6% exchange is seen under dehydrated conditions. 

While the complete dehydration of the zeolite does hinder ion exchange in the PEG solvents, the transition metal ions that are incorporated into the zeolite under dehydrated conditions are more catalytically active than those exchanged in the presence of trace water.  This is likely due to prevention of hydrolytic attack on the zeolite framework and metal hydroxide formation.  Catalytic efficiency toward NO decomposition was compared for Mn2+, Fe2+, and Co2+ exchanged Zeolite X samples prepared in aqueous solution and prepared in oligomer solvents.  Turnover frequencies for samples exchanged in PEG oligomers under dehydrated conditions (0.0237 s-1 for Na/Mn-X, 0.0213 s-1 for Na/Fe-X, and 0.0190 s-1 for Na/Co-X) are an order of magnitude higher than those exchanged in the presence of water.     

Exchange of rare earth ions having potentially useful luminescence properties was also explored.  Rare earth ions Nd3+ and Er3+ have been exchanged into hydrated and dehydrated Zeolite X using poly(ethylene glycol) oligomers as exchange solvents.  Under hydrated conditions, a maximum of 40% ion exchange was achieved, with the framework structure maintained through at least the first exchange cycle.  Although a maximum of only 8% ion exchange was observed under dehydrated conditions, structures were successfully maintained through several exchange cycles.  Luminescence and Raman spectroscopy studies indicate that ion exchange of RE3+ cations in aqueous solution leads to incorporation of the rare earth ions into the degraded framework, replacing Al3+ leached by the acidic exchange solution.  Ion exchange in PEG solutions prevents this process; the rare earth cations instead occupy the cation sites in the zeolite cages, leading to more optimal luminescence and highlighting the advantage of this method.