Laserfiche WebLink
Flood Control Levee August 24, 1999 Page <br />Taggart flood profiles. The actual freeboard for the n*prap is summarized ed on Table ; at several <br />locations, only 1. 8 feet of freeboard was achieved over the Taggart profile. Freeboard for the <br />designed ri rap over the base -flood profile ranges from 2.0 to 7.5 feet. <br />. f~ib rrnesh reinforced concrete cutoff wall was constructed at the toe of the South- Boulder - Creek <br />side of the levee from SCA station 106+00 to 135+30. It extends to a depth of three feet below the <br />elevation of the bottom of Dry Creek Ditch No. 23 which parallels the levee. No specifically - <br />constructed Filter layer is required. The typical section of the levee and -its erosion protection are <br />shown on the Ayres' as- constructed drawm* gs. <br />Certifications for the design and installation of the ri rap and cutoff wall are included with <br />Appendix 10. <br />CROSS SE TI OI <br />The cross section of the levee is a minimum often feet vide at the top, with a 0r�Nr_n_urn of :1 side <br />slopes on the interior and outside faces. The top vidth ofthe upstream reach averages 16.8 feet, with <br />a range of from ten to 23 feet. The side slopes average 3.9:1 on the outside slope and 3.5:1 on the <br />*Inside slope between S A stations 105+00 and 150+70. The cross sections for the upstream portion <br />of the upstream reach (station 1 3 5+00 to 1 50+70), and for the middle and downstream reaches, are <br />shown on a 9/27/96 SCA drawing (Appendix , For the remah f ng portion. of the upstream reach <br />between S CA stations 104 +0o and 1 +03 the final cross sections are shown on the 1998 Ayres as- <br />built drawings (Appendix 10. <br />INTERIOR DRAINAGE <br />The interior drainage facilities are shown on the Site Flan Map Figure 2 (and Appendix . Gravel <br />mining has created a large excavation north and west of the levee, which is about 12 feet below the <br />original grade. The whole site, however, falls about 45 feet in elevation from the south to the north. <br />The majority of the site behind the levee drains as overland flow, without being intercepted by any <br />specific drainage facility. The slope of the land is sufficient to move the water through and offthe <br />site. At the present, there are only a few drainage facilities on the site. All of them are operated by <br />gravity; none have any mechanical or electrical components. When the University develops the site <br />in the future, it is probable that it Will design and construct other drainage features behind the levee. <br />J stir am Reach <br />All of the surface drainage from the area behind the upstream reach of levee is generated from rain <br />falling on the immediate area, and on the adjacent area to the vest. The majority of the area behind <br />the upstream reach of levee drains northward as surface runoff without being intercepted by any <br />drainage facilities. A 1.9 -acre pond located near the middle of the site intercepts a small amount of <br />LEONARD RICE CONSULTING WATER ENGINEER S9 INC. <br />