Alafia River Minimum Flows and Levels - Southwest Florida Water ...
Alafia River Minimum Flows and Levels - Southwest Florida Water ...
Alafia River Minimum Flows and Levels - Southwest Florida Water ...
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Although Hickey (1998) concluded that climate was largely responsible for the<br />
decreasing trend, he did note that at the <strong>Alafia</strong> <strong>River</strong> at Lithia stream flow<br />
decreased about 44 cfs in the period between January 1962 to December 1981.<br />
He speculated that these flow declines were the result of mining, but were related<br />
to a substantial decrease in water being discharged rather than l<strong>and</strong>scape<br />
changes that resulted in hydrologic alterations. Decreases in discharge were<br />
accomplished through increased water use efficiency <strong>and</strong> a decrease in ground<br />
water usage. Inspection of water quality data for the river suggests that Hickey<br />
(1998) is correct, <strong>and</strong> flow declines are related to improved efficiency rather than<br />
a diminishment of flows resulting from l<strong>and</strong>scape alterations due to mining. In<br />
developing a relationship for the expressed purpose of predicting the impact of<br />
increasing area of phosphate mined l<strong>and</strong> on stream flow, SDI (2003) assumed<br />
that the trend of decreasing stream flow in the South Prong of the <strong>Alafia</strong> <strong>River</strong><br />
was related to increasing area of l<strong>and</strong> mined. This assumption was made<br />
because mining was essentially the only l<strong>and</strong> use that changed during the time<br />
interval investigated.<br />
While SDI (2003) assumed that the flow decline was attributable to increases in<br />
l<strong>and</strong> area mined for phosphate, this is not the case. Using logic similar to SDI<br />
(2003), there should be a steady monotonic decreasing trend in flow with<br />
increasing mined area. While mined area in the South Prong above the USGS<br />
gage increased substantially between 1972 <strong>and</strong> 1999 (from 9 to 72%) based on<br />
l<strong>and</strong> use maps for this time period (see Figure 2-21), flow remained fairly stable<br />
(Kendall's tau was run on mean annual flows for the period 1970 to 1999, <strong>and</strong> the<br />
slope of the Thiel line was –0.1918 with a p value of 0.8028; indicating no trend;<br />
see Figure 2-22).<br />
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