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The Determination of Minimum Flows for Sulphur Springs, Tampa

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DRAFT<br />

Lastly, the relationship between the indicator and flow should be quantifiable, so that<br />

change in the indicator can be expressed and used in determining the minimum flow<br />

rates.<br />

<strong>The</strong> District determined there are three management goals important to the<br />

establishment minimum flows <strong>for</strong> <strong>Sulphur</strong> <strong>Springs</strong>, which are: (1) minimize the incursion<br />

<strong>of</strong> high salinity water from the river into the upper spring run; (2) maintain low salinity<br />

habitats in the Lower Hillsborough River; and (3) provide a thermal refuge <strong>for</strong> manatees<br />

in the Lower Hillsborough River. <strong>The</strong> rationale and ecological indicators corresponding<br />

to <strong>for</strong> each <strong>of</strong> these goals are presented below. This discussion is based on the<br />

in<strong>for</strong>mation presented in Chapter 3 concerning the relationships <strong>of</strong> flow from <strong>Sulphur</strong><br />

<strong>Springs</strong> to the ecology <strong>of</strong> the spring run and Lower Hillsborough River.<br />

4.5 Goal 1 – Minimize the incursion <strong>of</strong> high salinity river water into the upper<br />

spring run.<br />

As discussed in Section 3.4, salinity data indicate that waters from the Lower<br />

Hillsborough River do not move into the upper spring run under normal flow conditions<br />

(no withdrawals). However, as flows are reduced by withdrawals, relatively high salinity<br />

water (up to 17 ppt) from the river can move into the upper spring run. Data collected by<br />

the FDEP and the FWC indicate that high salinity values that occurred in the upper<br />

spring run during the drought <strong>of</strong> 2000-2001 had a major impact on the<br />

macroinvertebrate community there, as a number <strong>of</strong> freshwater species were lost from<br />

the spring run. With the resumption <strong>of</strong> normal flows in late 2001, 2002 and 2003, a<br />

number <strong>of</strong> these species reappeared in the spring run, accompanied by increases in<br />

overall species richness, evenness, and diversity. A number <strong>of</strong> salt-tolerant species that<br />

persisted in the spring run during the drought also showed marked increases in<br />

abundance with the resumption <strong>of</strong> normal flows. Many <strong>of</strong> the species that rebounded<br />

with normal flows are important fish food organisms (isopods, amphipods, aquatic<br />

insects). Based on these findings, a goal <strong>of</strong> the District's minimum flow evaluation <strong>for</strong><br />

<strong>Sulphur</strong> <strong>Springs</strong> is to minimize the incursion <strong>of</strong> high salinity river water into the upper<br />

spring run. This goal should provide suitable conditions <strong>for</strong> many <strong>of</strong> the freshwater taxa<br />

that have been found in the spring run, and maintain the high species richness and<br />

diversity that was observed during periods <strong>of</strong> normal flow.<br />

When there are no incursions <strong>of</strong> river water, salinity values in the upper spring run<br />

typically vary between 1 and 3 ppt on a seasonal basis. Given this salinity range, the<br />

upper spring run would not be classified as fresh water (

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