Seasonal variations in natural organic matter and its impact on coagulation in water treatment

被引:221
作者
Sharp, Emma L. [1 ]
Parsons, Simon A. [1 ]
Jefferson, Bruce [1 ]
机构
[1] Cranfield Univ, Sch Water Sci, Cranfield MK43 0AL, Beds, England
基金
英国工程与自然科学研究理事会;
关键词
zeta potential; natural organic matter; coagulation; water treatment; charge density;
D O I
10.1016/j.scitotenv.2005.05.032
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In the past decade, a number of UK and US water utilities have been experiencing operational difficulties connected with the increased dissolved organic carbon (DOC) levels during the autumn and winter periods. This has been observed as an increase in the production of disinfection-by-products (DBP), and a greater coagulant demand. Resin adsorption techniques were used to fractionate raw water and investigate the variation in surface charge and coagulant-humic interactions over a 36-month period. A change in the natural organic matter (NOM) composition throughout the year was observed, with the fulvic acid fraction (FAF) increasing from 36% in September to 61% in November. However, a reduction in treatment performance is not simply due to an increase in DOC concentrations (from 4.3 to 14.5 mg L-1), but also a change in the charge density of the NOM. It was found that hydrophilic NOM fractions possess negligible charge density (< 0.06 meq g(DOC)(-1)), and it is the hydrophobic NOM fractions, FAF in particular, that exert the greater dominance on coagulation control. The hydrophilic NOM fractions are less amenable to removal through conventional coagulation with metal salts, and are therefore Rely to indicate the DOC residual remaining after treatment. Understanding the seasonal changes in NOM composition and character and their reactivity with coagulants should lead to a better optimisation of the coagulation process and a more consistent water quality. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:183 / 194
页数:12
相关论文
共 47 条
[1]  
AIKEN G, 2004, REMOVAL DISSOLVED OR
[2]  
Amirtharajah A., 1990, Water Quality and Treatment, American Water Works Association, V4th, P269
[3]   Interactions between natural organic matter (NOM) and membranes: Rejection and fouling [J].
Amy, G ;
Cho, J .
WATER SCIENCE AND TECHNOLOGY, 1999, 40 (09) :131-139
[4]  
AVNEA MJ, 1999, ENVIRON SCI TECHNOL, V32, P2739
[5]  
COLLINS MR, 1986, ENVIRON SCI TECHNOL, V20, P1026
[6]   REMOVAL OF DISSOLVED HYDROPHOBIC AND HYDROPHILIC ORGANIC-SUBSTANCES DURING COAGULATION FLOCCULATION OF SURFACE WATERS [J].
CROUE, JP ;
LEFEBVRE, E ;
MARTIN, B ;
LEGUBE, B .
WATER SCIENCE AND TECHNOLOGY, 1993, 27 (11) :143-152
[7]  
CROUE JP, 1993, AWWA WORKSH SEPT 16
[8]  
DENNETT KE, 1995, HUMIC SUBSTANCE REMO
[9]   Role of organic acidity in sorption of natural organic matter (NOM) to oxide surfaces [J].
Edwards, M ;
Benjamin, MM ;
Ryan, JN .
COLLOIDS AND SURFACES A-PHYSICOCHEMICAL AND ENGINEERING ASPECTS, 1996, 107 :297-307
[10]   COAGULATION IN DRINKING-WATER TREATMENT - PARTICLES, ORGANICS AND COAGULANTS [J].
EDZWALD, JK .
WATER SCIENCE AND TECHNOLOGY, 1993, 27 (11) :21-35