Strangled Waters: Second Wave

S. Levy
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Abstract

In August 2014, the water supply for the city of Toledo, Ohio, was poisoned. Officials issued an order to the half- million residents connected to the municipal water supply: Don’t drink, cook, or brush your teeth with the water. Do not use it to bathe your children, and don’t give it to your pets. Stores ran out of bottled water, and residents had to wait in long lines or travel to neighboring towns to find more. The culprit was a bright green plume of Microcystis, a cyanobacterium that thrives in warm water tainted with heavy loads of phosphorus and nitrogen. Every spring, rains wash a pulse of nutrients off fertilized fields and send it down the Maumee and Sandusky rivers and into western Lake Erie. Every summer, as water temperatures rise, Microcystis forms an iridescent mat over parts of the lake’s surface. In early August 2014, strong winds blew a lawn of cyanobacteria over Toledo’s water intake, which lies just outside the Maumee’s mouth. Tests showed that the city’s water contained dangerous levels of microcystin, a liver toxin produced by the bloom. The drinking water crisis was a dramatic signal of Lake Erie’s descent back into eutrophication. In the 1980s, after sewage plants in the watershed were upgraded and phosphate detergents banned, Lake Erie experienced a revival. Algal blooms faded, and populations of walleye rebounded. The lake grew a thriving tourist industry based on sport fishing. Then, in 1995, researchers recorded the lake’s first wide­spread bloom of Microcystis. Eruptions of Microcystis have since become a predictable event striking the western Lake Erie basin every summer. The most widespread and long- lasting blooms hit in 2011 and 2015, after intense spring rains dumped heavy loads of nutrients into the lake. Climate models forecast warmer summer temperatures and heavier spring rains for the Great Lakes region. Those conditions are a recipe for more and larger algal blooms, and are likely to favor Microcystis in particular. The regulatory efforts of the 1970s and 1980s made great progress in cleaning up discharges from industries and sewage treatment plants, but failed to address nonpoint source pollution flowing from farm fields and city streets.
窒息的水:第二波
2014年8月,俄亥俄州托莱多市的供水系统被污染。官员向与市政供水有关的50万居民发布命令:不要用水喝水、做饭或刷牙。不要用它给你的孩子洗澡,也不要给你的宠物。商店的瓶装水已经售罄,居民们不得不排长队等待,或者前往邻近的城镇寻找更多的瓶装水。罪魁祸首是一股亮绿色的微囊藻,这是一种蓝藻,在被大量磷和氮污染的温水中茁壮成长。每年春天,雨水从肥沃的土地上冲刷出一股养分流进莫米河和桑达斯基河,流入伊利湖西部。每年夏天,随着水温上升,微囊藻在部分湖面上形成彩虹色的垫子。2014年8月初,大风把一片蓝藻草坪吹到了托莱多的取水口上,就在莫米河口外。测试显示,该市的水含有危险水平的微囊藻毒素,这是一种由藻华产生的肝脏毒素。饮用水危机是伊利湖重新陷入富营养化的一个戏剧性信号。20世纪80年代,在流域内的污水处理厂升级,磷酸盐洗涤剂被禁用后,伊利湖经历了一次复兴。藻华逐渐消退,红眼鱼的数量开始回升。在钓鱼运动的基础上,这个湖发展出了繁荣的旅游业。然后,在1995年,研究人员记录了该湖第一次大范围的微囊藻爆发。自那以后,每年夏天,微囊藻的爆发已经成为伊利湖盆地西部发生的一种可预测的事件。最广泛和持续时间最长的水华发生在2011年和2015年,当时强烈的春雨将大量营养物质倾倒入湖中。气候模型预测,五大湖地区夏季气温升高,春季降雨增多。这些条件会导致更多更大规模的藻华,并可能特别有利于微囊藻。20世纪70年代和80年代的监管努力在清理工业和污水处理厂的排放方面取得了很大进展,但未能解决来自农田和城市街道的非点源污染。
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