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Effective April 28, 2015 Chapter Four Subsurface Sewage Treatment System Regulations <br />9.5 Soil observations. <br />Complete soil testing on each individual lot must be conducted prior to permit issuance independent of any prior <br />subdivision or lot approval testing. For permit issuance, a minimum of four (4) soil observations encompassing <br />the proposed sewage treatment area are required. At least one soil observation must be performed in the portion of <br />the soil treatment area anticipated to have the most limiting conditions. Larger areas may be required where <br />conditions of use, soils, topography, or vegetation require. Soil observations must comply with the following <br />requirements: <br />(1) The soil observation must be conducted within or on the borders of the proposed site; <br />(2) The soil observations must be performed in an exposed pit or by hand augering or probing. The use <br />of flight augers is not allowed; <br />(3) The soil observation method must allow observation of the different soil horizons that constitute the <br />soil profile and, if determining the loading rate by use of Table VI an undisturbed soil sample must <br />be observed; <br />(4) Underground utilities must be located before soil observations are undertaken; <br />(5) Required safety precautions must be taken before entering soil pits; <br />(6) Soil observations must be conducted prior to any required percolation tests to determine whether <br />the soils are suitable to warrant percolation tests and, if suitable, at what depth percolation tests <br />shall be conducted; and <br />(7) The minimum depth of the soil observations must be to the periodically saturated layer, to the <br />bedrock, or three feet below the proposed depth of the system, whichever is less. <br />9.6 Soil descriptions for determination of limiting layers. <br />Each soil profile observed at the proposed soil treatment and dispersal area must be evaluated under adequate light <br />conditions with the soil in a moist unfrozen state for the characteristics in items (1) through (8): <br />(1) The depth of each soil horizon measured from the ground surface. Soil horizons are differentiated <br />by changes in texture, color, redoximorphic features, bedrock, structure, consistence, and any other <br />characteristics that affects water movement or treatment of effluent; <br />(2) 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 <br />incorporated by reference, are available through the Minitex interlibrary loan system, and are not <br />subject to frequent change; <br />(3) A description of the soil texture, and structure using the United States Department of Agriculture <br />(USDA) soil classification system as specified in the Field Book for Describing and Sampling <br />Soils, which is incorporated by reference under Section 2.2 (46); <br />(4) Depth to bedrock. <br />(5) Depth to periodically saturated soil for new construction or replacement as determined by <br />redoximorphic features and other indicators, as determined in subitems (A) to (C): <br />(A) In subsoil and parent material, redoximorphic features include: <br />i. Distinct redoximorphic iron accumulation or distinct redoximorphic iron depletions; <br />ii. A gleyed or depleted soil matrix or redoximorphic mottles having a color chroma of <br />two or less or a depleted matrix or redoximorphic mottles having a color hue of 5Y <br />and a chroma of three or less; or <br />iii. Faint redoximorphic concentrations or faint redoximorphic depletions in subsoil or <br />parent material with a hue of 7.5YR or redder. <br />(B) In lower topsoil layers that are deeper than 12 inches from the surface and are immediately <br />followed in depth by a periodically saturated horizon, redoximorphic features include: <br />i. Soil colors with a redoximorphic chroma of two or less; or <br />ii. Redoximorphic accumulations or depletions. <br />(C) In the upper 12 inches of the topsoil layer, if it is immediately followed by a periodically <br />saturated horizon, the depth of seasonal saturation is determined by one or more of the <br />indicators in units (i) to (vi): <br />i. Soil colors with a chroma of zero; <br />35 Washington County Development Code <br />