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I <br />i <br />1 <br />1 <br />m <br />M <br />1 <br />1 <br />I <br />J <br />1 <br />i <br />m <br />I <br />4 <br />I <br />1 <br />I <br />The criteria of chroma less than 2 was not relied upon on this site since this 'ow chroma was <br />observed in definite upland areas which had clearly upland vegetation and no hydrology. <br />Wetland Hvdrologv <br />Hydrology on the site varied between standing water marshy areas to places that simply had <br />saturated soils throughout the basin. <br />The basins found to be non-wetland either had dr>- soils no different than the surrounding upland <br />areas (Basins 3, 11. 17, and 18). or had saniration only in the top 3 inches of the soil with dry soil <br />below (Basins 4, 10. and 13B). <br />Wetland Description <br />The site was reviewed in accordance with state and federally required delineation procedures <br />In the northwest comer of the site is Basin 1. a Type 1,2 Ag/Urban wetland (PEMIA) dominated <br />by reed canary grass. The basin is along the edge of the parcel. The adjacent upland on the <br />parcel is the soybean field and off the parcel is smooth brome grass. The NWl map shows a small <br />dot near this basin. <br />Basin 2 is a Type 2.3 Ag/Urban wetland (PEMIC) dominated by spikerush and cattail. This basin <br />is entirely within the soybean field and not found on the NWl map. There was adequate soil <br />saturation for this to be considered a wetland basin. <br />Basins 3 and 4 were found to be non-wetland due to lack of hydrology, soil characteristics, and the <br />marginal nature of the vegetation. Basin 3 is a: the head of a westward-flowing drainage ravine <br />where a drainage tile outlets the soybean field. The tile is greater than 2 feet below the ground <br />surface at the lowest point of this area; no gleying or mottling of the soil was observed here, nor <br />was the soil saturated. Vegetation consisted of giant ragweed, a smanweed species and <br />quackgrass. <br />Basin 4 did not appear on the NWl map and was cropped at the time of the 1/2 section aerial <br />photo. Tlie soil ill the basin was identical to that of the adjacent soybean field. While some <br />8