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Advances in Water Treatment and Enviromental Management

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ADSORPTION OF TRIHALOMETHANES ON TO ZEOLITES 183THM precursors are ill-def<strong>in</strong>ed macromolecular structures <strong>and</strong> their selective removalby adsorption can prove slow <strong>and</strong> difficult (Ram et al, 1986, p239). Dis<strong>in</strong>fectantsother than chlor<strong>in</strong>e may prove less effective <strong>and</strong>/or more expensive to use, eg ozone.Equally, precise control of the chlor<strong>in</strong>ation reaction is necessarily complex to copewith wide variations of feed conditions, without over or under dos<strong>in</strong>g (Ram et al,1986, p46).The use of adsorption as a method of remov<strong>in</strong>g THMs from dr<strong>in</strong>k<strong>in</strong>g water has anumber of advantages over the previous options. It can be applied as a discreteunit operation at the end of the treatment process, allow<strong>in</strong>g all other operations torema<strong>in</strong> unchanged. The process is generally superior to other removal techniquessuch as air stripp<strong>in</strong>g, distillation or biological treatment, <strong>in</strong> that it usually haslower capital <strong>and</strong> operat<strong>in</strong>g costs, <strong>and</strong> is more effective (O’Brien et al, 1983, pp337–362). Adsorption us<strong>in</strong>g powdered activated carbon (PAC) or granular activatedcarbon (GAC) is already <strong>in</strong> widespread use for this application, especially <strong>in</strong> theUSA. The ma<strong>in</strong> problem is the cost of regenerat<strong>in</strong>g the carbon once it is saturated(O’Brien et al, 1983, pp337–362). This can either be done <strong>in</strong> situ, requir<strong>in</strong>gmoderately expensive <strong>and</strong> complex plant, or the carbon is sent away forregeneration, <strong>and</strong> simply replaced with fresh stock.The purpose of this research project is to <strong>in</strong>vestigate the feasibility of us<strong>in</strong>g novelsynthetic crystall<strong>in</strong>e pentasil-zeolites such as silicalite (Flanigen <strong>and</strong> Grose,1977) <strong>and</strong> similar materials to adsorb THMs from dr<strong>in</strong>k<strong>in</strong>g water. Zeolites areporous crystall<strong>in</strong>e alum<strong>in</strong>osilicates consist<strong>in</strong>g of an assemblage of Si0 4 <strong>and</strong> Al0 4tetrahedra jo<strong>in</strong>ed by oxygen atoms to form a crystal lattice with pores ofmolecular dimensions. The pore size is precise <strong>and</strong> uniform, giv<strong>in</strong>g them theirhighly selective nature. The Si <strong>and</strong> A4 atoms are bound together with oxygenatoms, <strong>and</strong> <strong>in</strong> the case of the pentasil-zeolites, hav<strong>in</strong>g a structure based on adouble five r<strong>in</strong>g unit (Figure 1) which, stacked <strong>in</strong> a variety of ways, form different,but related, structures. The ZSM-5 structure is characterised by a r<strong>in</strong>g of tentetrahedra <strong>and</strong> may be prepared <strong>in</strong> a virtually alum<strong>in</strong>ium-free form known assilicalite.By vary<strong>in</strong>g the ratio of Si to Al from one up to about 100, the nature of thesynthesised material is greatly affected. At low Si/Al ratios the zeolites have a highaff<strong>in</strong>ity for polar molecules such as water, but at a Si/Al ratio of between eight <strong>and</strong>ten a transition normally occurs, <strong>and</strong> a hydrophobic nature is <strong>in</strong>troduced wherebythe material preferentially adsorbs organics rather than water. The uniform poresize of silicalite, at around 6 Angstrom units, limits this adsorption to lowmolecular weight organics only, mak<strong>in</strong>g the material potentially attractive for theselective removal of THMs from water (Shultz-Sibbel et al, 1982). The secondadvantage of zeolitic adsorbents is their high thermal stability <strong>in</strong> air up totemperatures of about 1100°C, permitt<strong>in</strong>g regeneration by simply heat<strong>in</strong>g <strong>in</strong> air, ascompared to the <strong>in</strong>ert atmosphere <strong>and</strong> closely controlled conditions necessary foractivated carbon regeneration.

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