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Wetland E: At 8.13 acres, Wetland E is the largest wetland in the RTC project area. <br />This wetland is located within a shallow, linear, drainage swale that bisects the west <br />central portion of the RTC project area. This entire wetland has been row cropped to <br />soybeans or corn during recent years. A total of 6.22 acres of Type 1 wetland will be <br />directly impacted though a combination of fill and conversion to stormwater ponds. The <br />remaining 1.91 acres will be retained within a proposed water way corridor and 6.22 <br />acres of Wetland E will require mitigation. <br />Lake Itasca: Lake Itasca and its direct drainage area are located approximately 1.2 <br />miles northwest of the RTC (Figure 12.1). A lake overflow elevation of 871 was <br />determined from a field survey of the area and two -foot contour information from <br />development plans. An analysis of lake elevations for the 100-year, 24-hour rainfall and <br />100-year, 10-day snowmelt events, show that Lake Itasca does not outlet from the low <br />point along the southeast side of the lake. This assessment held true for both existing and <br />future land uses. Lake levels do, however; rise to within a few one hundredths of a foot <br />for the 100-year, 10-day snowmelt event and within 1/2 foot for the 100-year, 24-hour <br />rainfall events. For this reason, the City of Ramsey has proposed installation of an outlet <br />for the lake. Since a DNR permit would be required for an outlet below the DNR OHW, <br />it has been assumed that any outlet would be above the OHW and above the 100-year <br />flood elevation of approximately 871.0 feet. This outlet would provide assurances that <br />existing and future homes will not be impacted by high water. No impacts to Lake Itasca <br />or adjacent wetlands are anticipated. <br />Mississippi River: The Mississippi River is located approximately 1/2 mile south of the <br />RTC. There currently is no outlet from the RTC to the River; all flow leaving the site <br />crosses Highway 10, flows to the southeast in a ditch, and eventually infiltrates. As <br />shown in Figure 17.2c, an overland waterway system is proposed to convey stormwater <br />south from the RTC to the Mississippi River. This waterway system would consist of a <br />series of water quality treatment ponds, infiltration ponds and constructed wetlands. As <br />discussed in Item 17 of this AUAR, a peak flow rate of 25.3 cfs is predicted under post - <br />development conditions for the 100-year storm event. For small events (1-year and less), <br />discharge ranges from 14.2 cfs, assuming no infiltration in the ponds, to 2.3 cfs when <br />infiltration is included. The outfall to the Mississippi River is proposed to follow a <br />County owned linear piece of land that extends from Highway 10 to the River (see Figure <br />12.5). The use of this property is not confirmed by the County at this time, but <br />discussions continue. If built, the outlet will consist of a 21-inch pipe, enlarged near the <br />Mississippi River to reduce velocities. Potential impacts include disturbance to the river <br />bluff line where the outfall pipe is installed and in -stream scour and erosion where the <br />pipe meets the river. If the County alternative outlet is not approved, an alternative <br />alignment along Highway 10 to the southeast, with a connection to the River will be <br />pursued. <br />Groundwater -Surface Water Interaction and Wetland Impacts <br />As part of the wetland delineation (Appendix A, NAWE Wetland Delineation Report) <br />completed for this AUAR, aerial photography for the period 1981 — 1996 was analyzed to <br />determine if any trends existed with respect changes in wetland hydrology. The aerial <br />12-3 <br />