Influence of eutrophication on the coagulation efficiency in reservoir water.

Water from the three reservoirs, Min-ter, Li-yu-ten and Yun-ho-shen, was examined for concentration of chlorophyll a, ultraviolet absorption (UV(254)), fluorescence intensity (FI), concentration of dissolved organic carbon (DOC), and fractionation of dissolved molecules by molecular weight. The water samples were collected over the change from spring to summer (May to July but before the typhoon season) when the water temperature and extent of eutrophication increase. Analytical results indicate that the concentration of DOC is proportional to the concentration of chlorophyll a, but not to the values of UV(254) and FI. Therefore, eutrophication, extraneous contaminants of small molecules, and the extracellular products of algae cause an increase in DOC, but a decrease in the proportion of large organic molecules such as of humic substances. The fraction of DOC with a molecular weight of less than 5000 Da increases with the concentration of chlorophyll a. All these data suggest that changes in the quality of water after eutrophication make the treatment of drinking water more difficult. The method of enhanced coagulation was recently developed for removing DOC. However, the results of this paper demonstrate that the efficiency of DOC removal falls as the degree of eutrophication increases. When the percentage of DOC with small molecules excreted by algae increased by 1%, the efficiency of DOC removal decreased by approximately 1%, implying that enhanced coagulation are not able to remove the DOC excreted by the algae during eutrophication, and resulting an increased concentration of trihalomethanes formation in water disinfections process.

[1]  James K. Edzwald,et al.  Aluminum Coagulation of Natural Organic Matter , 1990 .

[2]  H. Yeh,et al.  The effect of organic characteristics and bromide on disinfection by-products formation by chlorination , 1997 .

[3]  R. F. Christman,et al.  Identity and yields of major halogenated products of aquatic fulvic acid chlorination. , 1983, Environmental science & technology.

[4]  G. Amy,et al.  NOM characterization and treatability , 1995 .

[5]  Chihpin Huang,et al.  Interactions between alum and organics in coagulation , 1996 .

[6]  B. Logan,et al.  Molecular Size Distributions of Dissolved Organic Matter , 1990 .

[7]  S. D. Boyce,et al.  Reaction pathways of trihalomethane formation from the halogenation of dihydroxyaromatic model compounds for humic acid. , 1983, Environmental science & technology.

[8]  K. Pihlaja,et al.  Measurement of aquatic humus content by spectroscopic analyses , 2000 .

[9]  M. Edwards Predicting DOC removal during enhanced coagulation , 1997 .

[10]  Stephen J. Randtke,et al.  Formation of organic chlorine in public water supplies , 1983 .

[11]  A. P. Black,et al.  Review of the Jar Test , 1957 .

[12]  G. Amy,et al.  Comparing Gel Permeation Chromatography and Ultrafiltration for the Molecular Weight Characterization of Aquatic Organic Matter , 1987 .

[13]  W. Cheng Comparison of hydrolysis/coagulation behavior of polymeric and monomeric iron coagulants in humic acid solution. , 2002, Chemosphere.

[14]  Gary L. Amy,et al.  Molecular Size Distributions of Dissolved Organic Matter , 1992 .

[15]  G. Amy,et al.  Jar-test evaluations of enhanced coagulation , 1995 .

[16]  Mark C. White,et al.  Evaluating criteria for enhanced coagulation compliance , 1997 .

[17]  Mark LeChevallier,et al.  Impact of enhanced and optimized coagulation on removal of organic matter and its biodegradable fraction in drinking water , 2000 .

[18]  R. Perry,et al.  The significance of algae as trihalomethane precursors , 1998 .

[19]  K. Mopper,et al.  Fluorescence as a possible tool for studying the nature and water column distribution of DOC components , 1993 .

[20]  Richard A. Larson,et al.  Reaction Mechanisms in Environmental Organic Chemistry , 1994 .

[21]  Stuart W. Krasner,et al.  Predicting the Formation of DBPs by the Simulated Distribution System , 1991 .