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The Determination of Minimum Flows for Sulphur Springs, Tampa

The Determination of Minimum Flows for Sulphur Springs, Tampa

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DRAFT<br />

<strong>The</strong> experimental withdrawals ended on July 5, 2002 when high river flows returned to<br />

the spillway at the Hillsborough River dam. Due to an unusually wet year, there was<br />

nearly continuous river flow at the Hillsborough River through the remainder <strong>of</strong> 2002<br />

and all <strong>of</strong> 2003. Consequently, diversions <strong>of</strong> spring water to the base <strong>of</strong> the dam were<br />

not necessary to meet minimum flows at the dam. Additional experimental withdrawals<br />

to evaluate minimum flows <strong>for</strong> Sulfur <strong>Springs</strong> were also not conducted because the river<br />

was usually fresh near the spring mouth. Experiments that involved diverting various<br />

amounts <strong>of</strong> water to the base <strong>of</strong> the dam were conducted during the spring <strong>of</strong> 2004,<br />

during a two-month period when there was no flow from the reservoir. <strong>The</strong> findings <strong>of</strong><br />

these flow experiments will be included in the re-evaluation <strong>of</strong> the minimum flow <strong>for</strong> the<br />

Lower Hillsborough River scheduled <strong>for</strong> 2005.<br />

2.5.3 Concentrations and trends <strong>of</strong> other constituents<br />

Summary statistics <strong>for</strong> water quality parameters measured monthly in the spring pool by<br />

the City <strong>of</strong> <strong>Tampa</strong> are presented in Table 2-2 <strong>for</strong> the years 2001-2002. As is<br />

characteristic <strong>of</strong> Florida springs, the water in the spring pool typically has very low levels<br />

<strong>of</strong> color, turbidity, and total suspended solids. Total organic carbon and biochemical<br />

oxygen demand (BOD) concentrations are also low. Although water clarity is not<br />

measured in the pool, the water generally appears to be very clear, again typical <strong>of</strong><br />

spring discharge.<br />

<strong>The</strong> average temperature <strong>of</strong> the spring water is 25.1 degrees Celsius (77.2 degrees<br />

Fahrenheit), with only minor seasonal variation. <strong>The</strong>re are typically low levels <strong>of</strong><br />

dissolved oxygen in the spring pool; with a median concentration <strong>of</strong> 1.78 mg/l. Ground<br />

water discharges are frequently low in dissolved oxygen, and the occurrence <strong>of</strong><br />

dissolved oxygen in <strong>Sulphur</strong> <strong>Springs</strong> may be partly due to circulation and aeration that<br />

occurs within the spring pool. Photosynthesis by attached algae, which can become<br />

dense on the sides and bottom <strong>of</strong> the pool, may also contribute to high dissolved<br />

oxygen concentrations that are periodically observed.<br />

Nutrients in the spring pool are generally low, but do indicate some nutrient enrichment.<br />

<strong>The</strong> median nitrate nitrogen concentrations in the pool were 0.25 mg/l during 2001-<br />

2002, with an inter-quartile range (25 th to 75 th percentile) <strong>of</strong> 0.19 to 0.73 mg/l. <strong>The</strong><br />

median total nitrogen concentration was 0.72 mg/l, with inter-quartile range <strong>of</strong> 0.53 to<br />

1.45 mg/l. By comparison, Friedman and Hand (1989) reported a median concentration<br />

<strong>of</strong> 1.2 <strong>for</strong> total nitrogen in Florida streams, with values <strong>of</strong> 0.70 and 1.9 mg/l <strong>for</strong> the 20 th<br />

and 80 th percentiles, respectively. <strong>The</strong> median total phosphorus concentration <strong>for</strong><br />

<strong>Sulphur</strong> <strong>Springs</strong> (0.1 mg/l) was very similar to the median values reported <strong>for</strong> Florida<br />

streams (0.11 mg/l).<br />

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