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Volume 3 nr 1 / 2011 - Academia Oamenilor de Stiinta din Romania

Volume 3 nr 1 / 2011 - Academia Oamenilor de Stiinta din Romania

Volume 3 nr 1 / 2011 - Academia Oamenilor de Stiinta din Romania

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Two-dimensional Mo<strong>de</strong>lling of Acci<strong>de</strong>ntal Flood Wave Propagation 83STAGE 3: The bottom outflow pipe insi<strong>de</strong> plot 20 is damaged and, in a similarway as that of stage 2, plot 20, with a height of 80 m, will be <strong>de</strong>stabilized. Due tothe loss of the stabilizing filling, plot 20 becomes unstable, leans towards plot 18and starts sli<strong>din</strong>g. The water also flows through the bin<strong>din</strong>gs of plot 20 and 21. Atthe end of stage 3, plot 20 hours collapsed and the opening measures now 30 m inwidth. The discharge now reached the maximum value of 21700 m 3 /s.STAGE 4: During the last stage, the lake empties through the 30 m wi<strong>de</strong> and 80 mtall opening. Due to the <strong>de</strong>crease in the water volume, the discharge diminishesduring an 80 minute period, until the value of the discharge reaches its normalvalue (see fig. 9). Similar to scenario 1, the hydrograph of the breaking in scenario 2has a very fast growth time and the emptying of the lake ends 155 min after theacci<strong>de</strong>nt (see fig. 9). The two hydrographs for scenario 1 and 2 will constitute theboundary conditions for the 2D calculation.Fig. 8. Scenario 1 – Stage 1 and 2.Fig. 9. Scenario 2 – Discharge hydrograph.Copyright © Editura Aca<strong>de</strong>miei <strong>Oamenilor</strong> <strong>de</strong> Știință <strong>din</strong> România, <strong>2011</strong>Watermark Protected

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