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Changes in the quality of river water before,during and after a major flood event associated with a La Nina cycle and treatment for drinking purposes

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摘要 The treatment of organics present in the lower reaches of a major river system(the Murray–Darling Basin, Australia) before(March–July 2010), during(December 2010–May 2011) and after(April–December 2012) a major flood period was investigated. The flood period(over 6 months)occurred during an intense La Nia cycle, leading to rapid and high increases in river flows and organic loads in the river water. Dissolved organic carbon(DOC) increased(2–3 times) to high concentrations(up to 16 mg/L) and was found to correlate with river flow rates. The treatability of organics was studied using conventional jar tests with alum and an enhanced coagulation model(mEnCo). Predicted mean alum dose rates(per mg DOC) were higher before(9.1 mg alum/mg DOC) and after(8.5 mg alum/mg DOC) than during the flood event(8.0 mg alum/mg DOC),indicating differences in the character of the organics in raw waters. To assess the character of natural organic matter present in raw and treated waters, high performance size exclusion chromatography with UV and fluorescence detectors were used. During the flood period, high molecular weight UV absorbing compounds(〉2 kDa) were mostly detected in waters collected,but were not evident in waters collected before and afterwards. The relative abundances of humic-like and protein-like compounds during and following the flood period were also investigated and found to be of a higher molecular weight during the flood period. The treatability of the organics was found to vary over the three climate conditions investigated. The treatment of organics present in the lower reaches of a major river system(the Murray–Darling Basin, Australia) before(March–July 2010), during(December 2010–May 2011) and after(April–December 2012) a major flood period was investigated. The flood period(over 6 months)occurred during an intense La Nia cycle, leading to rapid and high increases in river flows and organic loads in the river water. Dissolved organic carbon(DOC) increased(2–3 times) to high concentrations(up to 16 mg/L) and was found to correlate with river flow rates. The treatability of organics was studied using conventional jar tests with alum and an enhanced coagulation model(mEnCo). Predicted mean alum dose rates(per mg DOC) were higher before(9.1 mg alum/mg DOC) and after(8.5 mg alum/mg DOC) than during the flood event(8.0 mg alum/mg DOC),indicating differences in the character of the organics in raw waters. To assess the character of natural organic matter present in raw and treated waters, high performance size exclusion chromatography with UV and fluorescence detectors were used. During the flood period, high molecular weight UV absorbing compounds(〉2 kDa) were mostly detected in waters collected,but were not evident in waters collected before and afterwards. The relative abundances of humic-like and protein-like compounds during and following the flood period were also investigated and found to be of a higher molecular weight during the flood period. The treatability of the organics was found to vary over the three climate conditions investigated.
出处 《Journal of Environmental Sciences》 SCIE EI CAS CSCD 2014年第10期1985-1993,共9页 环境科学学报(英文版)
基金 supported by a South Australian Premier's Science and Research Fund project‘Development of Materials Engineering Solutions for Treatment of Murray-Darling Basin Sourced Water Supplies’and the Australian Research Council through the ARC Linkage Project‘Materials Engineering Solutions for Tomorrow's Water Resources’,LP100100616
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