Laserfiche WebLink
were black mucky loam to 16 inches meeting the F1 indicator for hydric soil (loamy mucky <br /> mineral). Free water was observed at 10 inches below the soil surface in the sample borehole. <br /> Secondary indicators of wetland hydrology included geomorphic position and the FAC-Neutral <br /> Test. <br /> Adjacent upland at the sample location was dominated by Kentucky bluegrass with lesser <br /> amounts of smooth brome and Canada goldenrod. Soils at the upland transect location were <br /> black silty clay loam to 14 inches, underlain by black clay loam to 46 meeting the Al2 indicator <br /> for hydric soil (thick dark surface) (professional experience). No primary or secondary <br /> indicators of wetland hydrology were observed. <br /> The delineated boundary followed an abrupt change in vegetation composition and a slight <br /> change in topography. Wetland 1 corresponded to an NWI mapped PEMF/PEMC wetland and <br /> DNR Protected Wetland 842W,and an area mapped with hydric soils(Glencoe and Klossner)on <br /> the soil survey. Wetland 1 rated as a Mange 1 wetland based on on-site observations and our <br /> MnRAM analysis. <br /> Wetland 2 was a Type 1 (PEMAd)partially drained, fresh meadow wetland swale dominated by <br /> reed canary grass. Soils observed below the wetland boundary were black clay loam to 46 <br /> inches meeting the Al2 indicator for hydric soil (thick dark surface) (professional experience). <br /> No free water or saturated soils were observed in the sample borehole. Secondary indicators of <br /> wetland hydrology included geomorphic position and the FAC-Neutral Test. <br /> Adjacent upland at the sample location was dominated by Kentucky bluegrass with lesser <br /> amounts of Canada goldenrod and reed canary grass. Upland soils were black clay loam to 46 <br /> inches meeting the Al2 indicator for hydric soil(thick dark surface) (professional experience). <br /> No primary or secondary indicators of wetland hydrology were observed. <br /> The delineated boundary followed an abrupt change in vegetation composition and a slight <br /> change in topography. Wetland 2 did not correspond to any NWI mapped wetlands, but was <br /> located within an area mapped with very poorly drained,poorly drained, and somewhat poorly <br /> drained soils (Hamel-Glencoe)on the soil survey. Wetland 2 rated as a Mange 2 wetland based <br /> on on-site observations and our MnRAM analysis. <br /> Wetland 3 was a Type 1 (PEMA)fresh meadow wetland dominated by reed canary grass. Soils <br /> observed below the wetland boundary were black clay loam to 46 inches meeting the Al2 <br /> indicator for hydric soil(thick dark surface)(professional experience). No free water or <br /> saturated soils were observed in the sample borehole. Secondary indicators of wetland <br /> hydrology included geomorphic position and the FAC-Neutral Test. <br /> Adjacent upland at the sample location was dominated by Kentucky bluegrass with lesser <br /> amounts of Canada goldenrod and reed canary grass. Upland soils were black clay loam to 46 <br /> inches meeting the Al2 indicator for hydric soil(thick dark surface) (professional experience). <br /> No primary or secondary indicators of wetland hydrology were observed. <br /> 4 <br />