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I Holcim-WCR,Inc. I Morrison Quarry Drainage Report <br /> Appendix F—Hydraulics <br /> It's assumed the channel will be riprapped lined and have a geotextile to reduce risk of <br /> infiltration. <br /> The design flow for 100-year and 5-year return periods are estimated in Appendix E and are <br /> 25.4 cfs and 6.6 cfs respectively. <br /> Table 1 — Design Flow <br /> Return Interval <br /> 5-year 6.6 <br /> 100-year 25.4 <br /> Hydraulic Design Results <br /> The channel configuration along the bench is limited by the width of the inactive quarry bench. <br /> In concert with the geotechnical analysis the channel is proposed to have a bottom width of 2 <br /> feet, a constructed depth of 3 feet, side slopes of 2H:1V, and have a geotextile anchor trench <br /> along the reclaimed highwall with clay content material to mitigate potential infiltration of flows <br /> entering the channel. Details are presented in Appendix H — Design Drawings. <br /> The chute portion calculated by the NRCS workbook is identical to the bench except the bottom <br /> width is increased to 3 feet to ensure a commonly available D50 = 12 inch riprap material is <br /> stable. The results in the attached workbook and FlowMaster outputs are the basis of the design <br /> drawings presented in Appendix H. <br /> The superelevation of the flow in the chute portion is estimated using this USACE equation and <br /> a coefficient of 1.0 and design radius of 135 feet: <br /> ❑Y I.�Cl''T (8.8) <br /> Where; <br /> ❑Y _ Rise in water-surface elevation (superelevation) around the outside <br /> of a channel bend, in feet; <br /> C A coefficient (see Table 8.3); <br /> Y = Average velocity of flow, in feet per second; <br /> T — Channel width at elevation of water surface, in feet; <br /> g — Acceleration due to gravity (= 32.2 ft/sec2), <br /> rc = Radius of curvature of channel centerline, in feet; and, <br /> 1.5 — factor of safety to account For alluvial channel conditions. <br /> See U.S. Army Corps of Engineers (1970) for the source of this equation. <br />