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Mathematical Modeling of Unsteady Flow - Ameera Mohamad Awad - Bog

Mathematical Modeling of Unsteady Flowaf Ameera Mohamad Awad
Bag om Mathematical Modeling of Unsteady Flow

The study of the river flow predictions in open channels is an important issue in hydrology and hydraulics . Consequently, this paper is concerned with studying the unsteady flow that may exist in open channel , and its mathematically governed by the Saint Venant equation using a four-point implicit finite difference scheme. From many hydrologic software, HEC-RAS (Hydrologic Engineering Center ¿ River Analysis System) is a good choice to develop the hydraulic model of a given river system in the south of Iraq represented by Al- Kahlaa River by a network of main channel and three reach and a total of 57 cross sections with 3 boundary sections for one of the applications . The model was calibrated by using the observed weekly stage and flow data . The results show that a good agreement was achieved between the model predicted and the observed data by using the values Manning's(n=0.04) for over bank with the values of Manning's ( n=0.027) for main channel and also with using time weighting factor ( ¿ ) equal one .

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  • Sprog:
  • Engelsk
  • ISBN:
  • 9783330803732
  • Indbinding:
  • Paperback
  • Sideantal:
  • 148
  • Udgivet:
  • 22. november 2016
  • Størrelse:
  • 150x9x220 mm.
  • Vægt:
  • 238 g.
  • 2-3 uger.
  • 16. december 2024
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Beskrivelse af Mathematical Modeling of Unsteady Flow

The study of the river flow predictions in open channels is an important issue in hydrology and hydraulics . Consequently, this paper is concerned with studying the unsteady flow that may exist in open channel , and its mathematically governed by the Saint Venant equation using a four-point implicit finite difference scheme. From many hydrologic software, HEC-RAS (Hydrologic Engineering Center ¿ River Analysis System) is a good choice to develop the hydraulic model of a given river system in the south of Iraq represented by Al- Kahlaa River by a network of main channel and three reach and a total of 57 cross sections with 3 boundary sections for one of the applications . The model was calibrated by using the observed weekly stage and flow data . The results show that a good agreement was achieved between the model predicted and the observed data by using the values Manning's(n=0.04) for over bank with the values of Manning's ( n=0.027) for main channel and also with using time weighting factor ( ¿ ) equal one .

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