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Natural Organic Matter and Humic Substances Interactions

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4. Conclusions<br />

15th IHSS Meeting- Vol. 3<br />

This study examined the differential absorbance spectra of metal complexation with<br />

Suwannee River fulvic acid. While absorbance spectra show a very subtle change in intensity<br />

with increasing metal concentrations, they retain their characteristic featureless shape<br />

throughout the titrations. Differential absorbance spectra, on the other h<strong>and</strong>, show a number<br />

of features that are not present in the traditionally interpreted absorbance spectra. These<br />

features can be analyzed to reveal information about the nature of complexation-active<br />

chromophores in NOM. The differential absorbance spectra of SRFA can be successfully<br />

correlated to bound metal concentrations calculated based on the NICA-Donnan model<br />

theory. This study demonstrates that differential absorbance spectroscopy is a useful method<br />

to examine in situ the complexation behaviour of NOM. DAS can potentially provide detailed<br />

information about the emergence <strong>and</strong> contribution of different complexation-active functional<br />

groups <strong>and</strong> has the potential to elucidate the presence of functionalities which may not be<br />

detectable in traditional potentiometric experiments. In principle, this technique could allow<br />

the obtainment of detailed in situ information about NOM chemistry <strong>and</strong> reactivity caused by<br />

a wide variety of environmental <strong>and</strong> water treatment processes.<br />

References<br />

1. Korshin, G. V.et. al. Influence of NOM on copper corrosion,Journal of the American Water<br />

Works Association 1996, 88, 36–47.<br />

2. Edwards, M.; Sprague, N. <strong>Organic</strong> matter <strong>and</strong> copper corrosion by-product release: A mechanistic<br />

study,Corrosion Science 2001, 43, 1–18.<br />

3. Croue, J.-P.et. al. Isolation, fractionation, <strong>and</strong> characterization of natural organic matter in<br />

drinking water, AWWA Research Foundation, 2000.<br />

4. Leenheer, J. A.; Croue, J.-P. Characterizing aquatic dissolved organic matter,Environ. Sci.<br />

Technol. 2003, 37, 18A–26A.<br />

5. Stewart, A. J.; Wetzel, R. G. Fluorescence: Absorbance ratios –a molecular-weight tracer of<br />

dissolved organic matter,Limnol. Oceanogr. 1980, 25, 559–564.<br />

6. Del Vecchio, R.; Blough, N. V. On the origin of the optical properties of humic<br />

substances,Environ. Sci. Technol. 2004, 38, 3885–3891.<br />

7. Chin, Y.-P.et. al. Molecular weight, polydispersity, <strong>and</strong> spectroscopic properties of aquatic humic<br />

substances,Environ. Sci. Technol. 1994, 28, 1853–1858.<br />

8. Novak, J. M.et. al. Estimating the percent aromatic carbon in soil <strong>and</strong> aquatic humic substances<br />

using ultraviolet absorbance spectroscopy,J. Environ. Qual. 1992, 21, 144–147.<br />

9. Peuravouri, J.; Pihlaja, K. Molecular size distribution <strong>and</strong> spectroscopic properties of aquatic<br />

humic substances,Analytica Chimica Acta 1997, 337, 133–149.<br />

10. Dryer, D. J.et. al. In situ examination of the protonation behavior of fulvic acids using differential<br />

absorbance spectroscopy,Environ. Sci. Technol. 2008, 42, 6644–6649.<br />

11. Kinniburgh, D. G.et. al. Metal ion binding by humic acid: Application of the NICA-Donnan<br />

model, Environ. Sci. Technol. 1996, 30, 1687–1698.<br />

12. Benedetti, M. F.et. al. Metal ion binding by natural organic matter: From the model to the<br />

field,Geochim. Cosmochim, Acta 1996, 60, 2503–2513.<br />

Vol. 3 Page - 408 -

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