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�acobson Environmental, PLLC www.jacobsonenvironmental.com <br /> Environmental Consultants Wayne 7acobson, P.S.S.,W.D.C., P.W.S.,A.F.S. <br /> ------------------------------------------------------------------------------------------------------------ <br /> 5821 Humboldt Avenue North, Brookiyn Center, MN 55430 (612) 802-6619 Cell <br /> Email: jacobsonenv@msn.com <br /> A16 Coast Prairie Redox. A layer starting within 6 inches of the soil surface that is at least 4 inches <br /> thick and has a matrix chroma of 3 or less with 2 percent or more distinct or prominent redox <br /> concentrations occurring as soft masses and/or pore linings. <br /> User Notes: These hydric soils occur mainly on depressional landforms and portions of the intermound <br /> landforms on the Lissie Formation. Redox concentrations occur mainly as iron dominated pore linings. <br /> Common or many redox concentrations are required. Chroma 3 matrices are allowed because they may <br /> be the color of stripped sand grains or because few or common sand-sized reddish chert particles occur <br /> and may prevent obtaining chroma 2 or less. <br /> S1 Sandy Mucky Mineral. A layer of mucky modified sandy soil material 2 inches or more thick <br /> starting within 6 inches of the soil surface. <br /> User Notes: "Mucky" is a USDA texture modifier for mineral soils. The content of organic carbon is at <br /> least 5 percent and ranges to as high as 14 percent for sandy soils. The percent required depends on the <br /> clay content of the soil; the higher the clay content, the higher the amount of organic carbon required. An <br /> example is mucky fine sand, which has at least 5 percent but not more than about 12 percent organic <br /> carbon. <br /> S3 5 cm Mucky Peat or Peat. A layer of mucky peat or peat 2 inches or more thick with value of 3 <br /> or less and chroma of 2 or less, starting within 6 inches of the soil surface, and underlain by sandy soil <br /> material. <br /> User Notes: Mucky peat(hemic soil material)and peat(fibric soil material) have a minimum organic <br /> carbon content of 12 to 18 percent, depending on the content of clay. Organic soil material is called peat <br /> if virtually all of the plant remains are sufficiently intact to permit identification of plant remains. Mucky <br /> peat is at an intermediate stage of decomposition between peat and highly decomposed muck. To <br /> ascertain it mucky peat and/or peat are present, determine the percentage of rubbed fibers. <br /> S4 Sandy Gleyed Matrix. A gleyed matrix that occupies 60 percent or more of a layer starting <br /> within 6 inches of the soil surface. <br /> User Notes: Gley colors are not synonymous with gray colors. They are the colors on the gley color <br /> pages in the Munsell color book (Gretag-Macbeth, 2000). They have hue of N, 10Y, SGY, 10GY, 5G, <br /> 10G, 56G, 10BG, 56, 106, or 5P6 and value of 4 or more. For this indicator, the gleyed matrix only has <br /> to be present within 6 inches of the surface. Soils with gleyed matrices are saturated for periods of a <br /> significant duration; as a result, there is no thickness requirement for the layer. <br /> S5 Sandy Redox. A layer starting within 6 inches of the soil surface that is at least 4 inches thick <br /> and has a matrix with 60 percent or more chroma of 2 or less and 2 percent or more distinct or prominent <br /> redox concentrations occurring as soft masses and/or pore linings. <br /> User Notes: "DistincY' is defined as readily seen but contrast only moderately with the color to which <br /> compared. "ProminenY' is defined as contrasting strongly in color. Redox concentrations include iron and <br /> manganese masses (reddish mottles)and pore linings (Vepraskas, 1994). Included within the concept or <br /> redox concentrations are iron-manganese bodies occurring as soft masses with diffuse boundaries. <br /> Common (2 to less than 20 percent) or many (20 percent or more) redox concentrations are required <br /> (USDA, NRCS 2002). If the soil is saturated at the time of sampling, it may be necessary to let it dry to a <br /> moist condition for redox features to become visible. This is a very common indicator of hydric soils and <br /> is often used to identify the hydric/nonhydric soil boundary in sandy soils. <br /> Wetland Delineation-Mitigation-Permitting-Monitoring-Banking-Functional Analysis-T&E Surveys g <br /> Phase I Environmental Assessments-EAW's-Soil ID-Soil Analysis& Delineation-Environmental Referrals <br /> Pond &Lake Weed Control & Fish Stocking-Tree Surveys-Natural Resource Management Plans <br />