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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 87Implementation of the initial and boundary conditions. Mo<strong>de</strong>l calibration.The initial conditions refer to the overall calculation time and to the time step,parameters consi<strong>de</strong>red to be the global parameters of the mo<strong>de</strong>l. In the case ofPoiana Uzului pilot project, the overall calculation time was Tt = 40000 s, and thetime step t = 300 s. The boundary conditions are implemented at the inlet andoutlet of the mo<strong>de</strong>l and they are necessary for solving the equations system duringthe calculation.For the two scenarios an „inflow hydrograph” was introduced at the inlet of themo<strong>de</strong>l (fig. 15), and downstream, at the outlet of the mo<strong>de</strong>l, an „energetic slope”was <strong>de</strong>fined (fig. 16). Due to the non-existence of a similar inci<strong>de</strong>nt in the historyof the area, the calibration of the mo<strong>de</strong>l could not follow a real event. Thecalibration might have helped to obtain an accurate adjustment of the roughnesscoefficients. Due to the lack of such data, the calibration of the mo<strong>de</strong>l was notpossible. As mentioned before, the value of the roughness in the minor and majorriver bed was approximated on the basis of informations gathered during sitevisits and existing maps.Fig. 15. The inflow hydrograph at the inlet of the mo<strong>de</strong>l.Fig. 16. The outflow condition at mo<strong>de</strong>l exit.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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