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Heavy metal adsorption on iron oxide and iron oxide-coated silica ...

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133isotherm data (Figure 9.2). The results suggest that although polynuclear surfacecomplexes <strong>and</strong>/or precipitati<strong>on</strong> can account for isotherms with slopes not equal to <strong>on</strong>e(Lützenkirchen <strong>and</strong> Behra, 1994; Katz <strong>and</strong> Hayes, 1996), multisite <str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g> isapplicable when supported by spectroscopic data. More than <strong>on</strong>e type of surface site hasbeen experimentally observed <strong>on</strong> ferric oxyhydr<strong>oxide</strong> (Bottero et al. 1993) <strong>and</strong> supportedin crystallographic analysis (van Riemsdijk <strong>and</strong> Hiemstra, 1999). As Roberts<strong>on</strong> <strong>and</strong>Leckie (1997) note, even when slopes equal <strong>on</strong>e, this does not guarantee that <strong>on</strong>ly <strong>on</strong>etype of site is present; it is more likely that several site types exist.Even if site density is a functi<strong>on</strong> of pH, it appears that at least in this study, thehigh affinity site density falls within an order of magnitude of each other. Therefore, interms of applying the TLM, a single set of parameters describing both <str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g> edge<strong>and</strong> isotherm data would be more practical. Adsorpti<strong>on</strong> edges (Figure 9.3) are c<strong>on</strong>sistentwith isotherm data, the % Ni sorbed increased significantly from pH 5 to 6.5 at low Nic<strong>on</strong>centrati<strong>on</strong>s (Figure 9.3); however, at the highest [Ni]0 (Fig. 3a) the typical sigmoidcurve is not observed potentially due to site saturati<strong>on</strong>. All seven sets of TLM parametersderived from isotherms were used to predict edge data (Figure 9.3). Overall, <strong>on</strong>ly the pH6.5 set of parameters was found to predict all edge data reas<strong>on</strong>ably well (represented bythe solid line in each edge plot in Figure 9.3). These parameters were further tested <strong>on</strong>the isotherms, <strong>and</strong> results (Figure 9.4) indicate that this <strong>on</strong>e set of parameters successfullymodeled <str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g>. Therefore, a single set of TLM parameters was found to describe Ni<str<strong>on</strong>g>adsorpti<strong>on</strong></str<strong>on</strong>g> <strong>on</strong> goethite over a broad range of c<strong>on</strong>diti<strong>on</strong>s, covering almost seven orders ofmagnitude in c<strong>on</strong>centrati<strong>on</strong> (10 -10 to 10-3 M), i<strong>on</strong>ic strength from 10 -3 to 10-2, <strong>and</strong> anenvir<strong>on</strong>mentally relevant pH range from 5 to 6.5.

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