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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 81STAGE 2: Due to erosion on both si<strong>de</strong>s, plot 8, with a height of 65 m becomesunstable and leans towards plot 10, sli<strong>din</strong>g downstream in the same time; due toall this, water discharges also in between plots 8 and 7. At the end of stage 2, plot8 has fallen and the opening is 30 m wi<strong>de</strong>, the discharge reaching 18000 m 3 /s.STAGE 3: Due to si<strong>de</strong> erosions, plot 7, with a height of 55 m becomes unstableand leans towards plot 10, sli<strong>din</strong>g downstream in the same time (stage 6). At theend of this stage, plot 7 sli<strong>de</strong>s completely and collapses. At that point, the openingmeasures 45 m in width and the water discharge reaches the maximum value of22500 m 3 /s.STAGE 4: In this last stage, the lake empties through the 45 m wi<strong>de</strong> opening. Dueto the <strong>de</strong>crease in the water volume, the discharge diminishes during a period of110 minutes until it reaches the value of the normal discharge (see fig. 6). As youcan observe in figure 5, the hydrograph of the breaking has a very fast growth andthe emptying of the lake is completed in 148 minutes from the acci<strong>de</strong>nt.Fig. 4. Scenario 1 – Stage 1 and 2.Fig. 5. Scenario 1 – Stage 3 and 4.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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