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Tie-break Rule: Higher <br />Water Management <br />Water Management interpretations are tools for evaluating the potential of the soil in <br />the application of various water management practices. Example interpretations <br />include pond reservoir area, embankments, dikes, levees, and excavated ponds. <br />Retention Systems, Lined <br />Lined retention systems are stormwater management practices that are placed 3 to <br />5 feet in the ground, depending on the application. An impervious liner, made of <br />rubber or clay, is used to retain water and thus to maintain hydrophytic vegetation. <br />These systems are meant to be used where the hydrology will not allow other <br />systems, but the slope and bedrock depth are favorable. These systems include <br />retention basins and intermittent wetlands. They slow the movement of stormwater <br />to surface waters and also filter a significant portion of pollutants from the <br />stormwater. The fundamental function of these systems is to hold the runoff <br />generated by an area, such as a parking lot, from the first 1 inch of rainfall during a <br />24-hour storm preceded by 48 hours of no measurable precipitation. Water should <br />not be at the surface continuously, but a water table within the depth of the system <br />is needed to allow the growth of hydrophytic vegetation. Only that part of the soil <br />between depths of 24 and 80 inches is evaluated. <br />The ratings are based on the soil properties that affect infiltration of the stormwater, <br />construction and maintenance of the system, and public safety and health. Some <br />land shaping may be needed to allow stormwater runoff to accumulate in the <br />system. Saturated hydraulic conductivity (Ksat), depth to a water table, ponding, <br />depth to bedrock or a cemented pan, and flooding affect the transmission of <br />rainwater. Stones and boulders, ice, and bedrock or a cemented pan interfere with <br />installation. Subsidence interferes with installation and maintenance. Excessive <br />slope may cause lateral seepage and surfacing of the water in downslope areas. <br />Some slopes may become unstable and move upon addition of water <br />Soils that are underlain by loose sand and gravel or fractured bedrock at a depth of <br />less than 4 feet below the bottom of the system may adversely affect water quality <br />and public health. In these soils the lined retention system may not adequately filter <br />the stormwater, particularly if the adsorptive capacity of the soil below the system is <br />low. As a result, the ground water may become contaminated. In areas underlain by <br />limestone, solution channels and subsequent subsidence may damage adjacent <br />infrastructure. Also, areas underlain by limestone may be subject to ground-water <br />contamination. <br />The ratings are both verbal and numerical. Rating class terms indicate the extent to <br />which the soils are limited by all of the soil features that affect the specified system. <br />"Not limited" indicates that the soil has features that are very favorable for the <br />specified system. Good performance and very low maintenance can be expected. <br />"Somewhat limited" indicates that the soil has features that are moderately <br />favorable for the specified system. The limitations can be overcome or minimized by <br />Custom Soil Resource Report <br />46