Heavy metal adsorption on iron oxide and iron oxide-coated silica ...
Heavy metal adsorption on iron oxide and iron oxide-coated silica ...
Heavy metal adsorption on iron oxide and iron oxide-coated silica ...
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31• Underst<strong>and</strong> the effect of competing i<strong>on</strong>s <strong>on</strong> heavy <str<strong>on</strong>g>metal</str<strong>on</strong>g> <str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g> to ir<strong>on</strong><strong>oxide</strong>s. The ability of models developed in this research to predict heavy <str<strong>on</strong>g>metal</str<strong>on</strong>g>competiti<strong>on</strong> <strong>on</strong> ir<strong>on</strong> <strong>oxide</strong> will be tested.Specific hypotheses for this research include:First, surface functi<strong>on</strong>al groups <strong>and</strong> reacti<strong>on</strong>s are similar between crystalline <strong>and</strong>amorphous ir<strong>on</strong> <strong>oxide</strong>s (Davis <strong>and</strong> Leckie, 1978; Charlet <strong>and</strong> Manceau, 1993; Bargar etal. 1997b; Villalobos et al. 2001; Dixit <strong>and</strong> Hering, 2003). Therefore, XAS results for<str<strong>on</strong>g>metal</str<strong>on</strong>g> i<strong>on</strong>s sorbed <strong>on</strong> HFO may be applied to that <strong>on</strong> goethite. Bargar et al. (1997a, b)reported that ir<strong>on</strong> <strong>oxide</strong>s <strong>and</strong> aluminum <strong>oxide</strong>s have fundamentally similar crystalchemistry — both form Fe06 or A106 octahedra with very similar average Al-O <strong>and</strong> Fe-Ob<strong>on</strong>d lengths, therefore, they may exhibit comparable surface structures <strong>and</strong> functi<strong>on</strong>algroups. Bargar et al. (1997a, b) found that Pb(II) i<strong>on</strong>s sorbed as m<strong>on</strong><strong>on</strong>uclear bidentatecomplexes to edges of FeO6 or A1O6 octahedra <strong>on</strong> goethite, hematite, <strong>and</strong> aluminum<strong>oxide</strong>. Also, Pb <str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g> to HFO (three hours c<strong>on</strong>tact time) <strong>and</strong> 2-line ferrihydrite(Manceau et al. 1992; Scheinost et al. 2001; Trivedi et al. 2003 [for pH > 4.5]) weredominated by similar surface complexes. The first hypothesis will be tested by analyzingPb/HFO sorpti<strong>on</strong> samples (4 hours c<strong>on</strong>tact time) with XAS <strong>and</strong> comparing to that ofPb/goethite.Sec<strong>on</strong>dly, coupled with XAS data, intrinsic surface complexati<strong>on</strong> c<strong>on</strong>stants can beachieved by calibrating the SCM with a variety of <str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g> data including titrati<strong>on</strong>,isotherm, <strong>and</strong> edge data covering a wide range of c<strong>on</strong>diti<strong>on</strong>s. SCMs offer the advantageof representing surface chemical reacti<strong>on</strong>s with a set of quasi-thermodynamic c<strong>on</strong>stants,which are independent of changes in soluti<strong>on</strong> c<strong>on</strong>diti<strong>on</strong>s (Hayes, 1987). However, fewstudies have addressed both isotherm <strong>and</strong> edge data over a large range of c<strong>on</strong>diti<strong>on</strong>s withthe same model (e.g. Müller <strong>and</strong> Sigg, 1992; Waite et al. 1994; Heidmann et al. 2005);