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11-21-1977 Planning Packet
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11-21-1977 Planning Packet
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:areous till, <br />liar hills and <br />le original veg- <br />?d in Hennepin <br />relopment is dis- <br />diian green. This <br />lilltops. The <br />T, sidehill seep <br />ing wet seasons, <br />t rolling slopes <br />,e) is low to mod- <br />tely penr.eable. <br />ed periods. <br />diui!i green. Inis <br />The soil is well <br />eepage is not an <br />:s. The rolling <br />well (volune <br />. The soil is <br />left exposed for <br />mned in calcareous <br />ice. The native <br />’ one slope phase <br />Page -o- <br />> 1 <br />-T <br />■ >: <br />T-- <br />;!■ <br />Light <br />Green <br />5 <br />1 VV 5 <br />Dark <br />Blue <br />i' <br />ri <br />Nessel loam - 1 to 4 percent slope: <br />The map symbol for this soil is .N’eB and the map color is light green. This <br />soil is nearly level to gently sloping occupying areas of low relief and on <br />a few hilltops that are above Hayden soil on the side slopes. Since this <br />soil is nearly level little grading is generally required. <br />This soil is wet for short periods with a seasonal watertable at a 3 to 5 <br />foot depth. Shrink-swell (volume change) is low to moderate with changes <br />in moisture content. The soil is moderately pemeable. Soil strength is <br />adequate for residential development. <br />Marsh: <br />The map s>'mbol for this soil is Ma and the map color is dark blue. The <br />upper 5 to iO feet of the marsh is peaty muck or muck. This covers <br />other layers formed in vdiat was formerly a glacial lalce. The watertable <br />is near or above the surface the entire year. Tlicse soils liave very low <br />bearing capacity. The development characteristics of these soils are <br />generally unfavorable. These areas are best used for natural water stor <br />age and as scenic open space areas of developments. <br />rV. POTENTIAL OF SOILS FOR ON-SITE WLASTE TREABIENT <br />According to the recommended "Ordinance and Code Regulating Individual <br />Sewage Disposal Systems" published by the Minnesota Department of Health <br />in 1971 "No soil absorption system shall be installed in an area where <br />the watertable is at any time less than 6 1/2 feet below ground level <br />or 4 feet below the bottom of the drain field trench". <br />This line of thinking has changed somewhat over the past 6 years to re <br />flect research results conducted in various areas of the county. The <br />proposed Minnesota Pollution Control Agency ^^-40 "Individual Sewage <br />Treatment Systems Standards" states only that "The bottom of trenches <br />and beds shall be at least three feet above the watertable or bedrock" <br />and allows for installation of additional innovative systems other than <br />the standard subsurface trench system to meet this retiuirement. <br />/\n ex'ample of the innovative systems is the mound system. In the mound <br />system the seepage bed or trench is elevated by the use of sand fill to <br />provide the 3 foot separation distance between the bottom of the seepage <br />trench and a barrier laver such as the watertable or bedrock. <br />In the prelininaiy "Reconnnended Practices for On-Site Sewage Treatment <br />Systems" prepared by the City of Orono the 3 foot separation distance <br />is implied A\hen the highest point of groiindwater must be greater than <br />5 feet for installation of a standard soil absoi*ption system. <br />■r-i lb
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