Arsenic-sulfides confound anion exchange resin speciation of aqueous arsenic

A field-portable anion exchange resin method (often cited as the Ficklin method (1983)) has been extensively used to distinguish between dissolved arsenite (As(III)) and arsenate (As(V)) species in natural waters. As(III) occurs largely as As(OH) 3, which is uncharged at ca. pH 7, while As(V) is neg...

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Bibliographic Details
Published in:Water research (Oxford) Vol. 38; no. 5; pp. 1155 - 1158
Main Authors: Jay, Jenny Ayla, Keon Blute, Nicole, Hemond, Harold F., Durant, John L.
Format: Journal Article
Language:English
Published: Oxford Elsevier Ltd 01-03-2004
Elsevier Science
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Summary:A field-portable anion exchange resin method (often cited as the Ficklin method (1983)) has been extensively used to distinguish between dissolved arsenite (As(III)) and arsenate (As(V)) species in natural waters. As(III) occurs largely as As(OH) 3, which is uncharged at ca. pH 7, while As(V) is negatively charged and will sorb to the resin. However, we show that negatively charged As(III)-sulfide (thioarsenite) species, important at sulfide concentrations >10 μM, also bind to the anion exchange resins, and therefore might be interpreted incorrectly as As(V). Furthermore, we show that nitrogen-purging, which results in a conversion of As(III)-sulfides to arsenite, can be used to obtain accurate arsenic speciation when resins are used on sulfidic water samples.
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ISSN:0043-1354
1879-2448
DOI:10.1016/j.watres.2003.11.014