The Determination of Minimum Flows for Sulphur Springs, Tampa
The Determination of Minimum Flows for Sulphur Springs, Tampa The Determination of Minimum Flows for Sulphur Springs, Tampa
DRAFT There is evidence that flows have been gradually decreasing over time from Sulphur Springs. Daily flow records recorded by the United States Geological Survey (USGS) begin in 1956. Withdrawals from the spring pool began in the mid-1960s, but records for the withdrawals are unavailable for the period prior to 1984. For the period of 1984 to present, it is possible to correct the recorded flows on a monthly basis by adding back the quantities withdrawn. Consequently, the flow data prior to 1984 flow show much more scatter due to occasional low flows that are not corrected for withdrawals. Figure 2-19 shows time series plots of flows for both uncorrected pre-1984 data and 1984 to present data that are corrected for withdrawals. In both cases a Kendall-Theil regression line has been fitted to the data to illustrate the overall average trend. The Kendall-Theil method is a non-parametric form of regression that is independent of the data distribution and more robust in the presence of extreme values. The results of the regression for the two time periods are fairly similar and indicate a statistically significant (α = 0.05) slight decrease in flow over time. The slopes of the regression lines are –0.60 cfs/yr for the pre-1984 period and -0.36 cfs/yr for 1984 to present. 2.5 Water Quality of Sulphur Springs The water quality characteristics of the Sulphur Springs pool are described below. Seasonal and long-term trends in specific conductance are described first, since this parameter is a good indicator of the overall mineralization of the spring water and changes in the spring's ground-water sources. Periodic long-term specific conductance data from the USGS and the City of Tampa are evaluated with recent data from a continuous specific conductance recorder located in the spring pool. This is followed by a discussion of other water quality characteristics of the spring (e.g., nutrients, color), which are related to the ecological characteristics of the spring run and the adjoining reaches of the Lower Hillsborough River. 2.5.1 Data sources Water quality data for the Sulphur Springs pool examined in this report are taken from two sources. Since 1990, the City of Tampa has taken samples from Sulphur Springs pool for water quality analysis on a monthly basis. These data are submitted to the SWFWMD as part of the City’s water use permit for withdrawals from the spring. The USGS has also collected periodic water quality samples from the Sulphur Springs pool, with records dating back to the 1945 for some parameters. The frequency of sampling has varied considerably, ranging from a few measurements every several years prior to 1966 to roughly bi-monthly sampling during much of the 1970s and 1980s. Temperature, pH, specific conductance and dissolved oxygen have been the most frequently measured parameters. Water quality sampling by the USGS has decreased since the early 1990s, largely because regular water quality sampling was instituted by the City of Tampa. Selected variables in the USGS database are described as they compare to more recent data collected by the City. 2 - 19
DRAFT Figure 2-19 . Temporal trend of monthly Sulphur Springs flows: corrected and uncorrected for withdrawals. Kendall-Theil slope shown. 2 - 20
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- Page 16 and 17: Acronyms and Definitions DRAFT AMO
- Page 18 and 19: DRAFT Executive Summary The Southwe
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DRAFT<br />
<strong>The</strong>re is evidence that flows have been gradually decreasing over time from <strong>Sulphur</strong><br />
<strong>Springs</strong>. Daily flow records recorded by the United States Geological Survey (USGS)<br />
begin in 1956. Withdrawals from the spring pool began in the mid-1960s, but records <strong>for</strong><br />
the withdrawals are unavailable <strong>for</strong> the period prior to 1984. For the period <strong>of</strong> 1984 to<br />
present, it is possible to correct the recorded flows on a monthly basis by adding back<br />
the quantities withdrawn. Consequently, the flow data prior to 1984 flow show much<br />
more scatter due to occasional low flows that are not corrected <strong>for</strong> withdrawals.<br />
Figure 2-19 shows time series plots <strong>of</strong> flows <strong>for</strong> both uncorrected pre-1984 data and<br />
1984 to present data that are corrected <strong>for</strong> withdrawals. In both cases a Kendall-<strong>The</strong>il<br />
regression line has been fitted to the data to illustrate the overall average trend. <strong>The</strong><br />
Kendall-<strong>The</strong>il method is a non-parametric <strong>for</strong>m <strong>of</strong> regression that is independent <strong>of</strong> the<br />
data distribution and more robust in the presence <strong>of</strong> extreme values. <strong>The</strong> results <strong>of</strong> the<br />
regression <strong>for</strong> the two time periods are fairly similar and indicate a statistically significant<br />
(α = 0.05) slight decrease in flow over time. <strong>The</strong> slopes <strong>of</strong> the regression lines are –0.60<br />
cfs/yr <strong>for</strong> the pre-1984 period and -0.36 cfs/yr <strong>for</strong> 1984 to present.<br />
2.5 Water Quality <strong>of</strong> <strong>Sulphur</strong> <strong>Springs</strong><br />
<strong>The</strong> water quality characteristics <strong>of</strong> the <strong>Sulphur</strong> <strong>Springs</strong> pool are described below.<br />
Seasonal and long-term trends in specific conductance are described first, since this<br />
parameter is a good indicator <strong>of</strong> the overall mineralization <strong>of</strong> the spring water and<br />
changes in the spring's ground-water sources. Periodic long-term specific conductance<br />
data from the USGS and the City <strong>of</strong> <strong>Tampa</strong> are evaluated with recent data from a<br />
continuous specific conductance recorder located in the spring pool. This is followed by<br />
a discussion <strong>of</strong> other water quality characteristics <strong>of</strong> the spring (e.g., nutrients, color),<br />
which are related to the ecological characteristics <strong>of</strong> the spring run and the adjoining<br />
reaches <strong>of</strong> the Lower Hillsborough River.<br />
2.5.1 Data sources<br />
Water quality data <strong>for</strong> the <strong>Sulphur</strong> <strong>Springs</strong> pool examined in this report are taken from<br />
two sources. Since 1990, the City <strong>of</strong> <strong>Tampa</strong> has taken samples from <strong>Sulphur</strong> <strong>Springs</strong><br />
pool <strong>for</strong> water quality analysis on a monthly basis. <strong>The</strong>se data are submitted to the<br />
SWFWMD as part <strong>of</strong> the City’s water use permit <strong>for</strong> withdrawals from the spring.<br />
<strong>The</strong> USGS has also collected periodic water quality samples from the <strong>Sulphur</strong> <strong>Springs</strong><br />
pool, with records dating back to the 1945 <strong>for</strong> some parameters. <strong>The</strong> frequency <strong>of</strong><br />
sampling has varied considerably, ranging from a few measurements every several<br />
years prior to 1966 to roughly bi-monthly sampling during much <strong>of</strong> the 1970s and 1980s.<br />
Temperature, pH, specific conductance and dissolved oxygen have been the most<br />
frequently measured parameters. Water quality sampling by the USGS has decreased<br />
since the early 1990s, largely because regular water quality sampling was instituted by<br />
the City <strong>of</strong> <strong>Tampa</strong>. Selected variables in the USGS database are described as they<br />
compare to more recent data collected by the City.<br />
2 - 19