首页> 外文会议>International Symposium on Water-Rock Interaction(WRI-11) vol.2; 20040627-0702; Saratoga Springs,NY(US) >Origin, fate, and transport of ~(228)Ra and ~(226)Ra in groundwater and public drinking water, Pensacola, Florida, USA
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Origin, fate, and transport of ~(228)Ra and ~(226)Ra in groundwater and public drinking water, Pensacola, Florida, USA

机译:美国佛罗里达州彭萨科拉的地下水和公共饮用水中〜(228)Ra和〜(226)Ra的起源,命运和运输

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摘要

Over the past 50 years Pensacola, Florida has closed and abandoned a number of drinking water wells on which the city was dependent. The cause was traced chiefly to two industrial facilities within the city that are now designated as Superfund sites. One was a former wood treatment plant and the other a fertilizer manufacturing operation that was responsible for generation of a large groundwater plume containing elevated fluorine, aluminum, lead, arsenic, sulfate, and radium. The source of the latter was controversial but was ultimately traced to detrital monazite that was present in the heavy mineral fraction of ores shipped to, and processed at the site.
机译:在过去的50年中,佛罗里达州彭萨科拉关闭并放弃了该市赖以生存的许多饮用水井。原因主要归因于城市中的两个工业设施,现在被指定为超级基金所在地。一个是以前的木材处理厂,另一个是肥料制造厂,负责产生大量地下水,其中含有大量的氟,铝,铅,砷,硫酸盐和镭。后者的来源引起争议,但最终追溯到碎屑独居石,该碎屑独居石存在于运往现场并在现场加工的矿石的重矿物中。

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