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Lake Pocotopaug Lake and Watershed Restoration Evaluation ...

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The same analysis was performed with SDT <strong>and</strong> chlorophyll a values from 1991-2001, but usingCarlsons <strong>and</strong> Frink <strong>and</strong> Norvell data (Figure 16). Scatter was worse; data did not fit eithercurve. Reducing the data set to July <strong>and</strong> August values did not increase the correlation (Figure17). Data by year was plotted. 2001 appeared to follow the trend, but values were again shifteddown <strong>and</strong> to the left (Figure 18); indicating that <strong>Pocotopaug</strong> is exhibiting lower SDT based onchlorophyll a values. One could conclude that SDT is based more on non-algal turbidity.Total phosphorus <strong>and</strong> chlorophyll a values were plotted <strong>and</strong> compared to Carlson’s <strong>and</strong> Frink<strong>and</strong> Norvell’s data. Again, all 1991-2001 <strong>and</strong> July/August data produced much scatter (Figures19 <strong>and</strong> 20). 1991, 1993 <strong>and</strong> 2001 data were plotted separately (these are the only three yearswith chlorophyll a data). 2001 data provided the closest fit, although the slope was steeper thanCarlson or Frink <strong>and</strong> Norvell (Figure 21). The steeper upward trend indicates that there is morechlorophyll a than predicted by phosphorus concentrations. Algal density is higher thanexpected; algae are thriving in a lower phosphorus environment. However, more chlorophyll adata are needed to verify this trend.When comparing <strong>Lake</strong> <strong>Pocotopaug</strong> 2001 (TP between 10 <strong>and</strong> 20 ug/L) data to empirical modelspresented in literature, we find that average chlorophyll a in <strong>Lake</strong> <strong>Pocotopaug</strong> should bebetween 2.1 <strong>and</strong> 9.9 ug/L (Table 17). In 2001, <strong>Lake</strong> <strong>Pocotopaug</strong> average chlorophyll was 5.8ug/L, within the predicted average of the four empirical model calculations (3.1 – 7.6 ug/L).However, considering that average TP concentrations in 2001 were closer to the 10 ug/L (12<strong>and</strong> 13 ug/L), 2001 chlorophyll values are high compared to the empirical model predictions.Similarly, maximum chlorophyll values in <strong>Lake</strong> <strong>Pocotopaug</strong> were 11.7 <strong>and</strong> 14.8 ug/L at LP-1 <strong>and</strong>LP-2 respectively, within the 11.2 – 26.1 ug/L average maxima range. Indicating that <strong>Lake</strong><strong>Pocotopaug</strong> resembles most lakes at their worst condition (maxima are closer to measured<strong>Lake</strong> <strong>Pocotopaug</strong> values than averages). Average 2001 SDT was 2.01 m, below the predictedaverage for both 10 <strong>and</strong> 20 ug/L. Maximum 2001 SDT was 2.99 m, below predicted maxima.Using the average <strong>and</strong> maximum predicted chlorophyll, SDT was predicted using Carlson(1977) <strong>and</strong> Frink <strong>and</strong> Norvell (1984) calculations. Carlson’s average <strong>and</strong> maximum SDT rangedfrom 1.93 – 3.57 m <strong>and</strong> 0.84 – 1.49 m, respectively. Frink <strong>and</strong> Norvell average <strong>and</strong> maximumSDT ranged from 2.98 – 4.78 <strong>and</strong> 1.18 – 2.30 m, respectively. This indicates that if <strong>Lake</strong><strong>Pocotopaug</strong> behaved more like other lakes (reduce chlorophyll concentrations per unit TP),average SDT should be slightly lower than 3.57 <strong>and</strong> 4.78 m, with a worse case scenario ofslightly less than 1.49 – 2.30 m. Thus, increasing current average SDT by 1.5 m or greater,provided that SDT in <strong>Lake</strong> <strong>Pocotopaug</strong> is chl a driven.<strong>Lake</strong> <strong>Pocotopaug</strong> <strong>Restoration</strong> <strong>Evaluation</strong> 75May 2002

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