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equations (collectively referred to as the "empirical equations").1 The empirical equations predict <br /> the average breach width and failure time as a function of depth of water, dam height, and volume <br /> of water stored. For the outlet structure failure scenario the same three empirical methods were used <br /> to calculate failure time, but the average breach width was fixed at 52 feet for the North Dam, and <br /> 54 feet for the South Dam. Comparisons of the breach parameters calculated by each of the <br /> empirical equations for both breach scenarios are shown below in Table 1 and Table 2 for the <br /> North and South Dams, respectively. <br /> Table 1. Highland Reservoir No. 2 North Dam Failure <br /> Comparison of Dam Breach Parameters <br /> Empirical Method Average Breach Width Time of Failure <br /> (feet) (minutes) <br /> GROUND-LEVEL BREACH <br /> Froehlich 122 82 <br /> Von Thun and Gillette 113 80 <br /> USBR 63 13 <br /> BREACH INTO OUTLET CHANNEL <br /> Froehlich 52 64 <br /> Von Thun and Gillette 52 24 <br /> USBR 52 10 <br /> Table 2. Highland Reservoir No. 2 South Dam Failure <br /> Comparison of D am Breach Parameters <br /> Empirical Method Average Breach Width Time of Failure <br /> (feet) (minutes) <br /> GROUND-LEVEL BREACH <br /> Froehlich 89 113 <br /> Von Thun and Gillette 79 157 <br /> USBR 23 5 <br /> BREACH INTO HIGHLAND DITCH <br /> Froehlich 54 86 <br /> Von Thun and Gillette 54 42 <br /> USBR 54 11 <br /> 2.2 Dam Breach Simulation in HEC-HMS <br /> The U.S. Army Corps of Engineers' (USACE)hydrologic modeling computer program HEC-HMS <br /> was used to simulate clear-day piping failures of both of the Highland No. 2 Dams using the breach <br /> parameters estimated by each of the empirical equations. As a conservative measure,the simulation <br /> which produced the greatest peak outflow for each dam was selected for use in the downstream <br /> hydraulic modeling and inundation mapping. <br /> For each HEC-HMS breach simulation the water surface was set at the inlet ditch overflow crest <br /> (gage height 32) at the onset of the breach, and all water above the breach invert was assumed to <br /> drain. For the ground-level failure alternative the assumption was made that the breach would <br /> A fourth empirical method known as the MacDonald&Langridge-Monopolis/Washington State(2007) <br /> method was not considered based on recommendations found in the Guidelines for Dam Breach Analysis. <br /> HIGHLAND NO.2 NORTH AND SOUTH DAMS - 2 - June 15,2012 <br /> INUNDATION MAPPING REPORT <br />