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08/28/2006 Council Packet
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08/28/2006 Council Packet
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City Council
Council Document Type
Council Packet
Meeting Date
08/28/2006
Council Meeting Type
Regular
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• <br />• <br />Soderville Soil Series (continued) <br />The Ap horizon has hue of 10YR, value of 3 or 4, and chroma of 1 or 2. Undisturbed pedons have black <br />(10YR 2/1) or very dark gray (10YR 3/1) A horizons ranging from 2 to 6 inches thick. It is fine sand or <br />loamy fine sand. <br />The E horizon has hue of 10YR, value of 4 to 7, and chroma of 1 to 4. It is fine sand or loamy fine sand. <br />The Bt horizon has hue of 10YR or 7.5YR, value of 4 to 7, and chroma of 3 or 4. It is typically loamy fine <br />sand or loamy sand, but the range includes fine sand or sand with increase of content of clay. Fine sandy <br />loam and sandy loam are included as lamellae and total less than 3 inches in thickness. <br />The E &Bt horizon has colors and textures similar to the E and Bt horizons. This horizon consists of <br />multiple lamellae bands with intervening E horizons. <br />Some pedons have a C horizon with hue of 10YR, value of 4 to 6, and chroma of 2 or 3. It is fine sand or <br />sand. <br />COMPETING SERIES: There are no other series in this family. <br />GEOGRAPHIC SETTING: These soils have plane to slightly concave slopes. Slope gradients range <br />from 0 to 3 percent. The Soderville soils formed in deep sandy eolian or outwash sediments on outwash <br />plains. These sediments are of Wisconsin in age. Mean annual air temperature ranges from 38 to 45 <br />degrees F. Mean annual precipitation ranges from 24 to 30 inches. Frost free days range from 90 to 145. <br />The elevation above sea level ranges from 670 to 1450 feet. <br />GEOGRAPHICALLY ASSOCIATED SOILS: These are the Cantlin and Zimmerman soils. The <br />moderately well drained Cantlin soils occupy similar landscape positions, but do not have lamellae. The <br />excessively drained Zimmerman soils occupy higher landscape positions. <br />DRAINAGE AND PERMEABILITY: Moderately well drained. Runoff is negligible. Permeability is <br />rapid in the upper part and moderately rapid in the lower part. Soderville soils have a perched seasonal <br />high water table at a depth of 2.0 to 3.5 feet at some time from April to June in most years. <br />USE AND VEGETATION: Most areas of this soil are used for cropland. Common crops are corn, small <br />grain, and hay. Some areas are used as woodland. Common trees are jack pine, eastern white pine, red <br />pine, and northern red oak. <br />DISTRIBUTION AND EXTENT: East - central Minnesota. This soil is of small extent. <br />MLRA OFFICE RESPONSIBLE: St. Paul, Minnesota. <br />SERIES ESTABLISHED: Anoka County, Minnesota, 1972. <br />REMARKS: Diagnostic horizons and other features recognized are: ochric epipedon - the zone from the <br />surface to 30 inches (Ap, El, and E2 horizons); argillic horizon - the zone from 30 to 45 inches (Btl and <br />Bt2 horizons); <br />The Preserve Conservation Development - Restoration and Management Plan B -5 <br />
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