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<br />2.3 Past Analyses. _ <br />Twin Lake has been included in several past hydrologic studies. In the Hvdrolo is Anal sY is Of <br />Lakes and Open Space in Ramsey County (1975, Barr), overflow drainage from the Vadnais Lake <br />system is projected to flow into Twin Lake during severe rainstorms. This study described the outlet <br />control elevation for Twin Lake as being 874 feet MSL, and the lowest home's elevation as being at <br />876 feet. At such Time as the upstream watershed should be completely converted to urban-style Land <br />use, the 197 study projected a need for Twin Lake to be able to discharge 63 cfs in order for it not <br />to exceed a projected maximum allowable elevation of 875 feet. The report also recommended lowering <br />~ the outflow control elevation to 871 feet. <br />The Phalen Chain of Lakes Surface Water Management Plan (1988, Barr) describes Twin Lake's <br />position within the County Ditch 16 system. A detailed study of the lake's hydrology was not included, <br />but the report states that the lake will overflow to County Ditch 16 during very large storms or <br />snowmelt periods at an outflow rate of 63 cfs, based on the 1975 study. <br />Since the city of Vadnais Heights lies just to the north of Twin Lake, the lake is affected by water <br />management plans for that municipality. The Surface Water Management Plan for the City of Vadnais <br />Heights, developed by Short, Elliott & Hendrickson Engineering Company.(SEH) in 1989 shows Twin <br />Lake receiving overflow drainage from both the east and west portions of Vadnais Lake. Barr was not <br />able to verify an existing connection between the Twin Lake watershed and west Vadnais Lake during <br />this study. The SEH report asserts that a maximum of approximately 10 cfs will flow from Twin Lake <br />during the 100-year high-water event (assuming a high normal level, discussed below). <br />2.4 Water Quality Considerations <br />Twin Lake currently demonstrates water quality conditions that are good for a metropolitan lake. <br />This water quality owes largely to the regional topography and local geology which isolates the lake <br />hydrologically from nearby water bodies and watersheds. It currently receives runoff only from its own <br />watershed, which is small relative to the lake's volume. In addition, much of the lake's watershed <br />remains in its natural_ state, so that degradation of the Lake due to human activities has remained <br />minimal. The lake's present loading rate of pollutants and fertilizers is relatively low. <br />23162\264\TWINLAKE.RPT\I~h~i 3 <br />