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GLWMO MINUTES <br />JANUARY 24, 2008 <br />PAGE 9 <br />BMP analysis--management of curly leaf pondweed, internal loading sediment, a <br />shoreline restoration analysis to see if anything has been done to improve water quality of <br />the lake. Also, data was submitted to consultant D. Shapiro to look at any relationship <br />between the size of the lake and the number of zooplankton and water quality. <br />Preliminary findings show a lot of small zooplankton in the lake. A closer look is needed <br />because fish are not eating them. And analyze transparency by depth. <br />Mogg stated that the phosphorous models for this study and the one in 1991 are quite <br />different. This model shows a total of 626 pounds. The previous study showed 2,415 <br />pounds. Sobiech stated that one main difference is the amount of precipitation. Another <br />difference is that in the old study the calibrations are not as detailed as the present <br />models. When looking at the long-term record between 1994 and 2007, more unit runoff <br />per acre is measured per year of an area, which is compared to literature published data. <br />These models measure 6.5, which is right in the range where they are expected to be for <br />this type of watershed. When water volumes are backed out of the previous study, the <br />measurement is in the 10 to 12 range which could easily be accounted for in precipitation. <br />Stark stated that his concern is that 2007 was an abnormal year and, therefore, questions <br />the information. He asked if another year of samples should be taken. Sobiech stated <br />that it is important to monitor the southern site where only one storm event occurred and <br />at the Central Park east site. It would not be necessary to take samples again from the <br />north site. It is important to continue to monitor the west side of the lake where there is a <br />large drainage area. Other things that would be helpful would be to do periodic checks <br />on larger wetlands like Lake Judy, Lake Emily and Lake Bennett. How much water is <br />really infiltrating and discharging? More water is needed coming off the watershed than <br />rainfall which is impossible or need to have extreme groundwater rate into the lake which <br />doesn't seem possible. <br />Eckman noted a variable of tree maturity in phosphorous levels. Aichinger stated that <br />there are some variables in that lake monitoring data was not collected during leaf fall. It <br />was done in September. The trend will be seen in the spring. Sobiech stated that spring <br />concentration appears to be steady--20 to 30 micrograms per liter. If the plan is to collect <br />more data, he would hold off on further analysis. Otherwise, there maybe extensive <br />recalibrations. This is a good time to decide whether to hold off until more data is <br />collected or proceed with the data obtained and make those recommendations. <br />Aichinger stated that the concern is would recommendations from the current data <br />incorrectly assume internal loading be less of a factor. In a normal precipitation year, <br />that might not be seen and the BMPs would be totally different. <br />Stark asked how additional samples would fit the contract. Aichinger stated that the <br />contract would have to be modified with an extended timeline and the additional analyses <br />