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WSP11325
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Last modified
1/26/2010 3:16:59 PM
Creation date
10/12/2006 4:53:29 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8443.400
Description
Narrows Unit - Reports
State
CO
Basin
South Platte
Water Division
1
Date
3/1/1978
Author
Woodward-Clyde Consu
Title
Review Of Data And Studies Developed By The Bureau Of Reclamation For The Feasibility Stage Design Of Narrows Dam Colorado
Water Supply Pro - Doc Type
Report/Study
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<br />~ <br /> <br />Woodward.Clyde Consuhants <br /> <br />1 "U.' ') <br />v .,; <br /> <br />~ <br /> <br />4396. The profile drawing (Figure 2) indicates that the inter- <br /> <br />section of the active conservation and joint use reservoir <br /> <br />water levels with natural ground surface occurs around Stations <br /> <br />~ <br /> <br />229 and 230. The profile plots available to us may not <br />accurately show the ground surface. It is likely that the <br /> <br />foundation zone downstream from the dam around Stations 230 and <br /> <br />~ <br /> <br />232 will remain saturated to ground surface. We believe that <br /> <br />short term high water levels will create active steady-state <br /> <br />~ <br /> <br />seepage flow conditions at the toe of the dam. This <br /> <br />distribution of hydraulic gradients along the seepage paths <br /> <br />will not be uniform (at the average value) since foundation <br /> <br />soil permeabilities vary. A large portion of the loss in total <br /> <br />t <br /> <br />head will be near the exit zone, causing above average <br /> <br />hydraulic exit gradients. <br /> <br />Average hydraulic gradients are shown in Figure 8 for two <br /> <br />. <br /> <br />cross sections, Stations 231 and 224. The maximum average <br /> <br />gradient at Station 231 is 0.16 under maximum water surface <br /> <br />conditions. Considerable additional safety exists at Station <br /> <br />t <br /> <br />224 since natural ground level is about 15 feet above the <br /> <br />expected water surface (saturation surface) within the soil and <br /> <br />also because the resulting partially saturated zone in the <br /> <br />~ <br /> <br />foundation upstream and downstream of the embankment will <br /> <br />impede development of steady-state saturation flow conditions <br /> <br />during the brief periods that high water is against the <br /> <br />~ <br /> <br />embankment. In addition, the higher downstream ground surface <br /> <br />- 24 - <br /> <br />t <br /> <br />., <br />
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