Literature DB >> 25084347

Effects of iron on optical properties of dissolved organic matter.

Brett A Poulin1, Joseph N Ryan, George R Aiken.   

Abstract

Iron is a source of interference in the spectroscopic analysis of dissolved organic matter (DOM); however, its effects on commonly employed ultraviolet and visible (UV-vis) light adsorption and fluorescence measurements are poorly defined. Here, we describe the effects of iron(II) and iron(III) on the UV-vis absorption and fluorescence of solutions containing two DOM fractions and two surface water samples. In each case, regardless of DOM composition, UV-vis absorption increased linearly with increasing iron(III). Correction factors were derived using iron(III) absorption coefficients determined at wavelengths commonly used to characterize DOM. Iron(III) addition increased specific UV absorbances (SUVA) and decreased the absorption ratios (E2:E3) and spectral slope ratios (SR) of DOM samples. Both iron(II) and iron(III) quenched DOM fluorescence at pH 6.7. The degree and region of fluorescence quenching varied with the iron:DOC concentration ratio, DOM composition, and pH. Regions of the fluorescence spectra associated with greater DOM conjugation were more susceptible to iron quenching, and DOM fluorescence indices were sensitive to the presence of both forms of iron. Analyses of the excitation-emission matrices using a 7- and 13-component parallel factor analysis (PARAFAC) model showed low PARAFAC sensitivity to iron addition.

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Year:  2014        PMID: 25084347     DOI: 10.1021/es502670r

Source DB:  PubMed          Journal:  Environ Sci Technol        ISSN: 0013-936X            Impact factor:   9.028


  12 in total

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4.  Aeshnid dragonfly larvae as bioindicators of methylmercury contamination in aquatic systems impacted by elevated sulfate loading.

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5.  Association of dissolved organic matter characteristics and trace metals in mountainous streams with sabo dams.

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6.  Degradation potentials of dissolved organic carbon (DOC) from thawed permafrost peat.

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7.  Feasting on terrestrial organic matter: Dining in a dark lake changes microbial decomposition.

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8.  Iron influence on dissolved color in lakes of the Upper Great Lakes States.

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