海洋藻类对氯化河口水中三卤甲烷生成的贡献

Allan M. Crane , Stanton J. Erickson, Cynthia E. Hawkins
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引用次数: 5

摘要

利用代表浮游植物主要分类类群的三种海藻,即Isochrysis galbana (chrysophycea)、Carteria sp.(绿藻科)和thalassisira pseudonana(硅藻科),研究了天然存在的活藻叶绿素a在咸水氯化过程中产生三卤甲烷的潜力。对美国南卡罗来纳北部Edisto河的天然河口水(盐度为23 p.p.t)进行氯化处理,可快速生成201 ~ 221 μg的1−1三卤甲烷,主要由溴仿(CHBr3)和氯二溴甲烷(CHBr2Cl)组成。在106个ml−1的galbana细胞存在的情况下,用次氯酸钠(NaOCl)将过滤后的河口水氯化至名义10 mg 1−1的氯,使总三卤甲烷浓度平均增加41% (N = 6)。假海藻(thalassisira pseudonana)的存在使总三卤甲烷浓度平均下降24% (N = 6),而Carteria sp.对形成的总三卤甲烷浓度没有统计学上显著的影响。藻类培养物的叶绿素a含量与三卤甲烷浓度之间缺乏任何显著的统计相关性,这使我们不认为氯-叶绿素a相互作用是这些化合物的来源。然而,去除藻类种群后,藻类培养基氯化产生的三卤甲烷浓度表明,所观察到的三卤甲烷生产趋势主要是由于氯与藻类代谢副产物发生反应。
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Contribution of marine algae to trihalomethane production in chlorinated estuarine water

Three species of marine algae representing major taxonomic groups of phytoplankton, Isochrysis galbana (Chrysophyceae), Carteria sp. (Chlorophyceae), and Thalassiosira pseudonana (Bacillariophyceae), were utilized to investigate the potential of naturally occurring chlorophyll a of living algae to produce trihalomethanes during the chlorination of saline waters. Chlorination of filtered natural estuarine water (salinity=23 p.p.t.) from the North Edisto River, South Carolina, results in rapid formation of 201–221 μg 1−1 trihalomethanes comprised mainly of bromoform (CHBr3) and chlorodibromomethane (CHBr2Cl). In the presence of 106 cells ml−1 Isochrysis galbana, chlorination of filtered estuarine water with sodium hypochlorite (NaOCl) to a nominal 10 mg 1−1 chlorine increased the total trihalomethane concentration by an average of 41% (N = 6). The presence of Thalassiosira pseudonana resulted in an average 24% decrease (N = 6) while Carteria sp. did not produce a statistically significant effect upon the total trihalomethane concentration formed.

The absence of any significant statistical correlations between the chlorophyll a content of algal cultures and trihalomethane concentrations causes us to discount chlorine-chlorophyll a interactions as a source of these compounds. However, trihalomethane concentrations produced from the chlorination of algal culture media, after removal of algal populations, suggests instead that the observed trends in trihalomethane production are mainly due to chlorines reaction with the by-products of algal metabolism.

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