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AWWA WQTC69286
- Oxidation of Reduced Sulfur Specie (Thiosulfate) by Free Chlorine to Increase the Bed Life of Tailored GAC to Remove Perchlorate
- Conference Proceeding by American Water Works Association, 11/01/2008
- Publisher: AWWA
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This paper describes research into S<sub>2</sub>O<sub>3</sub><sup>2-</sup> oxidation bychlorine. Free chlorine was used as a pretreatment method to remove S<sub>2</sub>O<sub>3</sub><sup>2-</sup> from groundwater in Redlands, California. Chlorination in the form of hypochlorous acid(HOCl) and hypochlorite ion (OCl<sup>-</sup>) was used to oxidize S<sub>2</sub>O<sub>3</sub><sup>2-</sup> to sulfate prior totreatment with tailored granular activated carbon (TGAC). Thiosulfate, RSS, was seen tocompete with ClO<sub>4</sub><sup>-</sup> for adsorption sites on the TGAC. Experiments were first conductedsynthetically using deionized distilled (DI) water spiked with different concentration ofClO<sub>4</sub><sup>-</sup>, S<sub>2</sub>O<sub>3</sub><sup>2-</sup> and chlorine depicting a variety of treatment conditions. Conditions includeconcentrations of 1 and 0.5 mg/L ClO<sub>4</sub><sup>-</sup> and 1, 0.5 and 0.1 mg/L of S<sub>2</sub>O<sub>3</sub><sup>2-</sup>. Theseexperiments were carried out as pseudo reactions where free chlorine was in excess.Redlands groundwater was also spiked with S<sub>2</sub>O<sub>3</sub><sup>2-</sup>, the same concentration asbackground ClO<sub>4</sub><sup>-</sup> concentration that is found in the groundwater. Results showed that DIwater spiked with only 1 mg/L ClO<sub>4</sub><sup>-</sup> broke through at 15,000 bed volumes, while DIwater spiked with both 1 mg/L S<sub>2</sub>O<sub>3</sub><sup>2-</sup> and 1 mg/L ClO<sub>4</sub><sup>-</sup> broke through at 8,000 bedvolumes, representing a 47% capacity reduction. Moreover, deionized distilled water thatwas spiked with 1 mg/L ClO<sub>4</sub><sup>-</sup> and just a mere 0.1 mg/L S<sub>2</sub>O<sub>3</sub><sup>2-</sup> showed breakthrough at9,400 bed volumes, representing a 37% reduction. Next, the authors also pre-chlorinatedDI water with 0.25mg/L of free chlorine as HOCl, while this water also contained 1 mg/LClO<sub>4</sub><sup>-</sup> and 0.1 mg/L S<sub>2</sub>O<sub>3</sub><sup>2-</sup>; and in this case, ClO<sub>4</sub><sup>-</sup> broke through at 12,000 bed volumes.This indicates that chlorine oxidation of S<sub>2</sub>O<sub>3</sub><sup>2-</sup> increased the TGAC capacity to removeClO<sub>4</sub><sup>-</sup> from 63% to over 80%. As follow-up, Redlands groundwater that contained30 µg/L ClO<sub>4</sub><sup>-</sup> was spiked with 40 µg/L S<sub>2</sub>O<sub>3</sub><sup>2-</sup>, plus the 0.25 mg/L of HOCl. This RSSCTexhibited no difference for ClO<sub>4</sub><sup>-</sup> breakthrough between the RSSCT that was spiked,30,000 bed volumes, and the RSSCT that had no S<sub>2</sub>O<sub>3</sub><sup>2-</sup> present, 31,000 bed volumes.Significant difference in bed volumes to breakthrough was however observed whenS<sub>2</sub>O<sub>3</sub><sup>2-</sup> was more than 10 times greater than the ClO<sub>4</sub><sup>-</sup> concentration. The TGAC capacityto remove ClO<sub>4</sub><sup>-</sup> decreased to 17% and 50% when S<sub>2</sub>O<sub>3</sub><sup>2-</sup> concentration was 250µg/L and1mg/L respectively. Results to date suggest that S<sub>2</sub>O<sub>3<