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The Determination of Minimum Flows for Sulphur Springs, Tampa

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DRAFT<br />

apparently declined over time. Studies per<strong>for</strong>med by the City <strong>of</strong> <strong>Tampa</strong> in 1958<br />

confirmed a connection between <strong>Sulphur</strong> <strong>Springs</strong> and Curiosity Sink and also Blue Sink,<br />

which are located approximately 2.5 miles (4 km) northwest <strong>of</strong> <strong>Sulphur</strong> <strong>Springs</strong>. Tracer<br />

dyes indicated flow rates in the range <strong>of</strong> 4,200 to 9,200 ft per day (1,280 to 2,800<br />

meters per day). Stewart and Mills (1984) visited the Blue Sink complex in 1963-64 and<br />

noted that the sinks were approximately 20 to 30 feet (6.1 to 9.1 m) deep with water<br />

visibly flowing at the bottom. However, by 1981 the sinks were only about 6 feet (1.8 m)<br />

deep and dry. <strong>The</strong> connection between <strong>Sulphur</strong> <strong>Springs</strong> and the Blue Sink complex had<br />

been lost due to the build up <strong>of</strong> trash and sediment, which effectively plugged the sinks.<br />

A dye test was conducted by the City <strong>of</strong> <strong>Tampa</strong> in 1987 to determine if the connection<br />

still remained between Blue Sink and <strong>Sulphur</strong> <strong>Springs</strong>. <strong>The</strong> dye never arrived at the<br />

spring indicating that the connection was sealed.<br />

Figure 2-17. Known sinkholes locations near <strong>Tampa</strong>, Florida.<br />

In 1989, Environmental Engineering Consultants, Inc. conducted additional dye tracer<br />

tests to verify the hydraulic connection between Alaska and Poinsettia (also called<br />

Jasmine or Trinity) sinks to <strong>Sulphur</strong> <strong>Springs</strong>. Alaska sink is approximately 549 m (1,800<br />

ft) northwest <strong>of</strong> <strong>Sulphur</strong> <strong>Springs</strong> and Jasmine is 7,500 feet (2,286 m) north <strong>of</strong> <strong>Sulphur</strong><br />

<strong>Springs</strong>. <strong>The</strong> calculated flow rate <strong>for</strong> the flow between Alaska sink and <strong>Sulphur</strong> <strong>Springs</strong><br />

was 12,900 ft per day (3,932 meters per day). <strong>The</strong> results <strong>for</strong> the Poinsettia sink<br />

indicated a flow rate <strong>of</strong> approximately 8,200 ft per day (2,499 meters per day). <strong>The</strong> test<br />

derived flow rates are, <strong>of</strong> course, head dependent. <strong>The</strong> greater the hydraulic gradient<br />

the more pronounced the flow. Consequently, if levels are reduced at <strong>Sulphur</strong> <strong>Springs</strong><br />

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