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The Determination of Minimum Flows for Sulphur Springs, Tampa

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DRAFT<br />

For the evaluation <strong>of</strong> minimum flows, it is important to view the effects <strong>of</strong> withdrawals<br />

from <strong>Sulphur</strong> <strong>Springs</strong> on a short-term basis. To illustrate patterns <strong>of</strong> daily withdrawals<br />

from the spring during very dry periods, average daily pumpage values are plotted <strong>for</strong><br />

1999 - 2002 in Figure 2-11. <strong>The</strong> flat shape <strong>of</strong> the top <strong>of</strong> the pumpage hydrograph<br />

reflects series <strong>of</strong> consecutive days when the withdrawals were taken continuously at the<br />

pump capacity <strong>of</strong> 20 mgd (31 cfs). <strong>The</strong> most prolonged period <strong>of</strong> pumping from the<br />

spring occurred during May though July 2000, with frequent but less consistent pumping<br />

occurring during the first part <strong>of</strong> 2001.<br />

When they have occurred, withdrawals by the City <strong>of</strong> <strong>Tampa</strong> have had a major effect on<br />

flows from the spring pool to the spring run. <strong>The</strong> capacity <strong>of</strong> the pump (20 mgd) is<br />

almost as great as the average flow <strong>of</strong> <strong>Sulphur</strong> <strong>Springs</strong> (22 mgd or 34 cfs), and until<br />

recently, pumpage by the City <strong>of</strong> <strong>Tampa</strong> <strong>of</strong>ten caused flow to the spring run to fall to<br />

zero or very low rates <strong>of</strong> flow. Average daily flows from spring to the run are shown <strong>for</strong><br />

the 1999-2002 period in Figure 2-12. Comparison to Figure 2-11 shows that when<br />

withdrawals were in effect, discharges from the pool fell to very low values. When<br />

withdrawals ceased, there was a rapid increase in discharge from the spring pool.<br />

<strong>The</strong> period <strong>of</strong> high flow (> 50 cfs) that occurred primarily in 1999 was due to opening <strong>of</strong><br />

the gate at the spring outlet. During this period, the City opened the structure to lower<br />

water levels in the pool so that work on the swimming pool in the <strong>Sulphur</strong> <strong>Springs</strong> Park<br />

could be undertaken without damaging the structure <strong>of</strong> the swimming pool. Raising the<br />

gate and lowering water levels in the spring pool induces greater ground-water<br />

discharge due to less head pressure over the spring vent. In the spring <strong>of</strong> 1999, the City<br />

closed the structure and began withdrawals <strong>for</strong> water supply, as shown by the drop in<br />

flows seen in April though June <strong>of</strong> that year (Figure 2-12). Additional in<strong>for</strong>mation on the<br />

ground-water relations and flow characteristics <strong>of</strong> <strong>Sulphur</strong> <strong>Springs</strong> are presented in later<br />

sections <strong>of</strong> this report.<br />

2.3.1 Recent improvements to the diversion facilities at <strong>Sulphur</strong> <strong>Springs</strong><br />

Modifications were made to the water diversion facilities associated with <strong>Sulphur</strong><br />

<strong>Springs</strong> during 2001 to allow <strong>for</strong> better management <strong>of</strong> flows from the spring pool. As<br />

part <strong>of</strong> the minimum flow rule <strong>for</strong> the Lower Hillsborough River that was adopted in the<br />

year 2000, it was established that diversions from <strong>Sulphur</strong> <strong>Springs</strong> could be used to<br />

provide the 10 cfs minimum flow at the base <strong>of</strong> the Hillsborough River dam. To<br />

accomplish this objective, a junction was put in the pipe that leads from <strong>Sulphur</strong> <strong>Springs</strong><br />

to the reservoir so that spring waters can be released to the lower river near the base <strong>of</strong><br />

the dam. A valve and flow meter were installed at this junction so that varying amounts<br />

<strong>of</strong> spring water could be diverted either into the reservoir or to the base <strong>of</strong> the dam. A<br />

100 ft. long flume was constructed that extends from this junction to the river below the<br />

dam (Figure 2-13). <strong>The</strong> turbulence created by this flume aerates the spring water be<strong>for</strong>e<br />

it is released to the lower river.<br />

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