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<br />I <br /> <br />I <br /> <br />I <br /> <br />seepage, and drawdown from spillway elevation are stated ln Reference- <br />7 as 1.3, and 1.2, respectively. If an earthquake value of 0.1 g is <br />used, then the minimum factor of safety is 1.0, except for the drawdown <br />condition which shows that the existing embankment does not meet sug- <br />gested safety factors (i.e., 1.43 less than 1.50 without earthquake). <br /> <br />I I <br /> <br />I <br /> <br />I <br /> <br />B. Seepage Analysis <br />Some amount of seepage will occur through essentially all earth dams. <br />The problems arise when the amount of seepage affects the stability of <br />the dam and/or the quantity of seepage is excessive from the water value <br />standpoint. The potential seepage problem, with respect to stability, <br />was identified by the SED during several inspections. The .effect of the <br />seepage on the stability at the existing embankment was investigated ln <br />the previous section of this report, by varying those stability <br />parameters affected by permeability (i.e., cohesian, and 0 angle). <br />During the investigation of alternative improvements (Section V-C), <br />the design of the improvements included the effect of the existing <br />seepage conditions and other factors. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Due to the value of the water, however, the magnitude of the <br />seepage is an important consideration. If the quantity is sufficient <br />to justify the expense of reducing the amount, then the alternative <br />improvements should include provisions for minimizing the quantity. <br />There are several ways of estimating seepage quantities, including <br />energy or mass balance techniques, flow-net approximations, or direct <br />measurements. The energy and mass balance techniques require extensive <br />amounts of field data over a long period of time, and therefore were not <br />within the scope-of-work of this analysis. Direct measurements were not <br />practical due to the site constraints and physical limitations (i.e., <br />the seepage was not confined as to the source or to the discharge loca- <br />tion). Therefore, the flow-net approximation was selected due to the <br />simplicity of the method. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />-20- <br />