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Agenda - Council - 05/13/2014
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Agenda - Council - 05/13/2014
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Council
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05/13/2014
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25 INDIVIDUAL SUBSURFACE SEWAGE TREATMENT SYSTEMS 7080.1720 <br />D. underground utilities must be located before soil observations are undertaken; <br />E. required safety precautions must be taken before entering soil pits; <br />F. soil observations must be conducted prior to any required percolation tests to determine <br />whether the soils are suitable to warrant percolation tests and, if suitable, at what depth percolation tests <br />shall be conducted; and <br />G. the minimum depth of the soil observations must be to the periodically saturated layer, to <br />the bedrock, or three feet below the proposed depth of the system, whichever is less. <br />Subp. 5. Soil descriptions for determination of limiting layer. Each soil profile observed at the <br />proposed soil treatment area must be evaluated under adequate light conditions with the soil in a moist <br />unfrozen state for the characteristics in items A to H: <br />A. the depth of each soil horizon measured from the ground surface. Soil horizons are <br />differentiated by changes in texture, color, redoximorphic features, bedrock, structure, consistence, and any <br />other characteristic that affects water movement or treatment of effluent; <br />B. a description of all soil colors for each horizon according to the Munsell Soil Color Charts, <br />Revised Edition, Munsell Color Corporation (1992), or equivalent. The color charts are incorporated by <br />reference, are available through the Minitex interlibrary loan system, and are not subject to frequent change; <br />C. a description of the soil texture, structure, and consistence using the United States <br />Department of Agriculture (USDA) soil classification system as specified in the Field Book for Describing <br />and Sampling Soils, which is incorporated by reference under part 7080.1100, subpart 36; <br />D. depth to the bedrock; <br />E. depth to the periodically saturated soil for new construction or replacement as determined <br />by redoximorphic features and other indicators, as determined in subitems (1) to (3): <br />(1) in subsoil and parent material, redoximorphic features include: <br />(a) distinct redoximorphic iron accumulations or distinct redoximorphic iron <br />depletions; <br />(b) a gleyed or depleted soil matrix or redoximorphic mottles having a color chroma <br />of two or less or a depleted matrix or redoximorphic mottles having a color hue of 5Y and a chroma of three <br />or less; or <br />(c) faint redoximorphic concentrations or faint redoximorphic depletions in subsoil <br />or parent material with a hue of 7.5YR or redder; <br />(2) in lower topsoil layers that are deeper than 12 inches from the surface and are <br />immediately followed in depth by a periodically saturated horizon, redoximorphic features include: <br />(a) soil colors with a redoximorphic chroma of two or less; or <br />(b) redoximorphic accumulations or depletions; <br />(3) in the upper 12 inches of the topsoil layer, if it is immediately followed by a <br />periodically saturated horizon, the depth of seasonal saturation is determined by one or more of the <br />indicators in units (a) to (f): <br />(a) soil colors with a chroma of zero; <br />(b) organic soil textures or mineral soil textures with an organic modifier; <br />Copyright ©2014 by the Rev <br />so <br />of Statutes, State of Minnesota. All Rights Reserved. <br />
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