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Alafia River Minimum Flows and Levels - Southwest Florida Water ...

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While elevated phosphorus concentrations in streams can potentially be ascribed<br />

to numerous sources (e.g., waste water treatment plant discharges, some<br />

industrial discharges, fertilizer applications by agriculture or from residential<br />

areas), there can be little doubt that the elevated concentrations seen in the<br />

<strong>Alafia</strong> <strong>River</strong> from approximately 1960 (when routine water quality analysis began)<br />

to the early to mid 1980's are directly associated with phosphate mining activities<br />

in the watershed. Most of this mining (89%) has occurred in the sub-basins of<br />

the North <strong>and</strong> South Prongs. Supporting data are seen in elevated<br />

concentrations of a number of other chemical constituents, for example fluoride<br />

(an element commonly found in association with phosphate). Beginning in the<br />

mid-1970's, there is a rather sudden decline in phosphorus <strong>and</strong> other chemical<br />

constituents found in association with phosphate ore (e.g., fluoride, silica). This<br />

decline is graphically apparent (see Figure 2-34). Concomitant declines in<br />

fluoride <strong>and</strong> phosphorus are evidence of a change in mining practices that lead<br />

to dramatic reductions in phosphorus (<strong>and</strong> other constituent) loading to the <strong>Alafia</strong><br />

<strong>River</strong> system around 1975-1980.<br />

Unfortunately, there are no long-term records of in-stream phosphorus<br />

concentrations at the three gage sites prior to phosphate mining in the watershed<br />

(this is true of the upper Peace <strong>River</strong> also – see SWFWMD 2002). It is therefore<br />

difficult to determine if current in-stream concentrations approach those that<br />

would have been expected absent mining impacts. While there has been a<br />

considerable decrease in loading (perhaps an order of magnitude or more),<br />

concentrations of phosphorus (the majority of which is in the most biologically<br />

available form, phosphate) are still high when compared to most natural stream<br />

systems. Friedemann <strong>and</strong> H<strong>and</strong> (1989) determined the typical ranges of various<br />

constituents found in <strong>Florida</strong> lakes, streams <strong>and</strong> estuaries. Based on their<br />

finding, 95% of all <strong>Florida</strong> streams exhibited total phosphorus concentrations less<br />

than 1.99 mg/l P. The 1990 to 1999 decade mean for the <strong>Alafia</strong> <strong>River</strong> at Lithia is<br />

2.54 mg/l P (the median is 2.40) which despite large decreases in concentration<br />

still places it among the rivers with the highest P concentrations in the state.<br />

Similar trends in instream phosphorus concentrations are also evident in the<br />

Peace <strong>River</strong> (SWFWMD 2002). As with the <strong>Alafia</strong> <strong>River</strong>, these elevated levels<br />

were also attributable to past mining practices <strong>and</strong> discharges from related<br />

chemical processing plants. Similarly to the <strong>Alafia</strong> <strong>River</strong>, dramatic decreases in<br />

P concentration also occurred in the Peace <strong>River</strong> (Figure 2-35, although they<br />

occurred a few years later (around the mid-1980s) than at Lithia. Like the <strong>Alafia</strong><br />

<strong>River</strong>, other constituents found in association with phosphate also followed<br />

similar trends in concentration (e.g., fluoride – see Appendix) <strong>and</strong> similar declines<br />

as phosphate mining practices changed.<br />

2-70

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