Abstract
A strategy of research combining intense field monitoring and compartment modeling was used to characterize fluoride cycling in the semi-arid area around a newly installed aluminum factory in southern Argentina. The factory started operations In 1974 and emitted about 500 tons of gaseous fluorides to the atmosphere up to October 1976. Emphasis of research was on sedimentary or detritus cycling; periodically, samples were obtained from plant tissues, soils, sea water, and sea sediments. A compartment model of fluoride circulation at the atmosphere-vegetation interface provides further elements to Interpret the tendencies observed in field data. A fluoride budget up to October 1976 is presented showing the relative importance of environmental compartments monitored, with reference to fluoride accumulation. Plants are transient accumulators of atmospheric fluorides; soils, sea-water, and sea-sediments are sinks of the cycle. The major pathway of fluoride from terrestrial environment to coastal sea water Is along transportation with superficial soil eroded by wind. According to data here presented, it can be concluded that one wind storm can transport enough soluble fluorides to coastal waters to account for the transient differences of concentration observed.