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The Determination of Minimum Flows for Sulphur Springs, Tampa

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CHAPTER 5<br />

RESULTS OF THE MINIMUM FLOWS ANALYSES<br />

DRAFT<br />

5.1 Introduction<br />

This chapter presents the technical findings that support the recommended minimum<br />

flow <strong>for</strong> <strong>Sulphur</strong> <strong>Springs</strong>. <strong>The</strong> determination <strong>of</strong> the minimum flow was based on the<br />

degree that it met the three management criteria that were described in the previous<br />

chapter, which are: (1) maintain low salinity habitats in the spring run; (2) maintain low<br />

salinity habitats in the lower Hillsborough River, and (3) maintain a thermal refuge <strong>for</strong><br />

manatees. <strong>The</strong> findings related to these three criteria are presented sequentially below.<br />

5.2 Criterion 1 – Maintain low salinity habitats in the upper spring run<br />

As discussed in Section 3.4, the background salinity in the upper spring run in the<br />

absence <strong>of</strong> spring water withdrawals is determined primarily by the salinity <strong>of</strong> the<br />

discharge from <strong>Sulphur</strong> <strong>Springs</strong> pool. Under these normal flows, the background low<br />

salinity habitat <strong>of</strong> the upper spring typically ranges from 1 to 3 ppt (Figure 3-5). By<br />

reducing flow from the pool, withdrawals can raise salinity values in the spring run by<br />

allowing the movement <strong>of</strong> brackish water from the lower river into the upper spring run.<br />

Depending on the salinity tolerances <strong>of</strong> the species occurring in the spring run, such<br />

salinity incursions may, or may not, affect the species composition and ecology <strong>of</strong> the<br />

spring run.<br />

<strong>The</strong> most conservative way to maintain the low salinity characteristics <strong>of</strong> the upper<br />

spring run would be to keep spring flow above a flow rate that hydraulically prevents<br />

salinity incursions. However, if salinity incursions were infrequent and <strong>of</strong> short duration,<br />

they may not result in adverse impacts to the biota <strong>of</strong> the spring run. <strong>The</strong> determination<br />

<strong>of</strong> the criterion 1 minimum flow thus focused on the probability that various rates <strong>of</strong> flow<br />

from the spring would result in salinity incursions and the level and duration <strong>of</strong> such<br />

incursions.<br />

5.2.1 Criterion 1 data sources<br />

Two types <strong>of</strong> measured data provided an empirical basis <strong>for</strong> identifying the Criterion 1<br />

minimum flow. <strong>The</strong>se were a set <strong>of</strong> controlled spring release experiments conducted by<br />

the District during 2001 and 2002, and the multi-year continuous recorder data<br />

measured in the spring and river system by the USGS. <strong>The</strong> time periods <strong>of</strong> the<br />

experiments and continuous recorder data represent conservative periods <strong>of</strong> unusually<br />

low rainfall and were thus ideally suited <strong>for</strong> these analyses.<br />

5.2.2 Controlled release experiments<br />

<strong>The</strong> District measured salinity at 21 stations in the upper spring run during a set <strong>of</strong><br />

controlled spring release experiments conducted between November 2001 and June<br />

2002. During these experiments, the City <strong>of</strong> <strong>Tampa</strong> diverted variable amounts <strong>of</strong> water<br />

from <strong>Sulphur</strong> <strong>Springs</strong> pool to either into the Hillsborough River Reservoir or to the base<br />

5 - 1

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