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<br />D, SUMMARY OF AVAILABLE DATA <br /> <br /> <br />Appendix B provides a complete set of water quality data collected to <br /> <br /> <br />date on the reservoir, Due to the relative young age of the reservoir <br /> <br /> <br />(constructed by the Army Corps of Engineers in 1979) a limited set of <br /> <br /> <br />data exists on the reservoir. The Colorado Department of Health has <br /> <br /> <br />been collecting data during the past year as part of the Bear Creek <br /> <br /> <br />Water Quality Study and will continue to monitor during the next year, <br /> <br /> <br />funding permitting. <br /> <br /> <br />The water quality monitoring program for the reservoir includes the <br /> <br /> <br />collection of physical, chemical and biological data at sites in the <br /> <br /> <br />reservoir and tributary sampling, Three sampling locations were <br /> <br /> <br />determined by the Health Department with two samples collected per site <br /> <br /> <br />at the 0-2 meter photic zone and the other a composite of the remaining <br /> <br /> <br />water column, Sampling was established semi-weekly from July through <br /> <br /> <br />September and monthly from October through June. <br /> <br /> <br />Major conclusions drawn from the data are: <br /> <br />1. The reservoir becomes stratified during the summer months with <br /> <br /> <br />dissolved oxygen levels dropping to 0 mg/L below 5 meters. Thermal <br /> <br /> <br />stratification occurs during the summer at shallow depths, often the <br /> <br /> <br />thermocline developes just below the surface or at depths of less than 2 <br /> <br /> <br />meters. The thermal and oxygen stratifications are strong and the <br /> <br /> <br />shallow depths of occurance suggest the inflows are not mixing with the <br /> <br /> <br />lake water and short circuiting is occuring. This surface "sheet flow" <br /> <br /> <br />may be responsible, in part, for the lack of mixing and low dissolved <br /> <br /> <br />oxygen levels at relative shallow depths. <br /> <br />23 <br />