BibTex RIS Kaynak Göster
Yıl 2015, Cilt: 36 Sayı: 3, 2143 - 2152, 13.05.2015

Öz

Kaynakça

  • Yong G. Lai., Two-dimensional depth-averaged flow modeling with an unstructured hybrid mesh, Hydraulic Engineer, Sedimentation and River Hydraulics Group, Technical Service Center, Bureau of Reclamation, Denver, CO 80225
  • Edom Mesesse Moges.,Evaluation of Sediment Transport Equation and Parameter Sensitivity Analysis Using the SRH-2D, 2010
  • Yong G. Lai., “ 2D Flow Modeling with SRH_2D”., Hydraulic Engineer, Sedimentation and River Hydraulics Group, Technical Service Center
  • Yang C. T., Sediment Transport Theory and practice,1996
  • Vanoni, American society of civil engineers, sedimentation engineering,1975
  • Tolossa H. G.,Comparison of 2D hydrodynamic models in river reaches of ecological importance: Hydro-AS-2D and SRH_2D.2008
  • Van Rijn L. C., Sediment transport: Part 1 bed load transport, 1987
  • Lai Y. G., Theory and user manual for SRH_2D version-2,2008
  • Duan, j,G and Chen, Li(2003) Review of Sediment Transport Models, Technical Report, Desert Research Institute.71 pages.

Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model

Yıl 2015, Cilt: 36 Sayı: 3, 2143 - 2152, 13.05.2015

Öz

Abstract. One-dimensional (1D) flow models have been routinely used in practical hydraulic applications. Example models include HEC_RAS (Brunner, 2006), MIKE11 (DHI, 2002), CCHE1D (Wu and Vieira, 2002), and SRH_1D (Huang and Greimann, 2007). These 1D models will remain useful, particularly for applications with a long river reach (more than 50 km) or over a long time period (over a year). Their limitation, however, are well known and there are situations where multi-dimensional modeling is needed. For most river flows, water depth is shallow relative to width and vertical acceleration is negligible in comparison with gravity. So the two-dimensional (2D) depth-averaged model provides the next level of modeling accuracy for many practical open channel flows. Indeed, time has been ripe that 2D models may be routinely used for river projects on a personal computer. A range of 2D models have been developed and applied to a wide range of problems since the work of chow and Ben-Zvi (1973). The ability of a 2D model to solve open channel flows with complex geometries has always been a thrust for improvement as it is relevant to practical applications. In this report hydrodynamic and Sediment Transport Equations and Sensitivity Parameter Using the  Model are introduced.

Kaynakça

  • Yong G. Lai., Two-dimensional depth-averaged flow modeling with an unstructured hybrid mesh, Hydraulic Engineer, Sedimentation and River Hydraulics Group, Technical Service Center, Bureau of Reclamation, Denver, CO 80225
  • Edom Mesesse Moges.,Evaluation of Sediment Transport Equation and Parameter Sensitivity Analysis Using the SRH-2D, 2010
  • Yong G. Lai., “ 2D Flow Modeling with SRH_2D”., Hydraulic Engineer, Sedimentation and River Hydraulics Group, Technical Service Center
  • Yang C. T., Sediment Transport Theory and practice,1996
  • Vanoni, American society of civil engineers, sedimentation engineering,1975
  • Tolossa H. G.,Comparison of 2D hydrodynamic models in river reaches of ecological importance: Hydro-AS-2D and SRH_2D.2008
  • Van Rijn L. C., Sediment transport: Part 1 bed load transport, 1987
  • Lai Y. G., Theory and user manual for SRH_2D version-2,2008
  • Duan, j,G and Chen, Li(2003) Review of Sediment Transport Models, Technical Report, Desert Research Institute.71 pages.
Toplam 9 adet kaynakça vardır.

Ayrıntılar

Bölüm Derleme
Yazarlar

Edris Merufınıa

Saeed Judı Sanı Bu kişi benim

Shoja Nourı Bu kişi benim

Yayımlanma Tarihi 13 Mayıs 2015
Yayımlandığı Sayı Yıl 2015 Cilt: 36 Sayı: 3

Kaynak Göster

APA Merufınıa, E., Judı Sanı, S., & Nourı, S. (2015). Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi, 36(3), 2143-2152.
AMA Merufınıa E, Judı Sanı S, Nourı S. Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi. Mayıs 2015;36(3):2143-2152.
Chicago Merufınıa, Edris, Saeed Judı Sanı, ve Shoja Nourı. “Evaluation of Hydrodynamic and Sediment Transport Equations and Parameter Sensitivity Analysis Using the SRH_2D Model”. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi 36, sy. 3 (Mayıs 2015): 2143-52.
EndNote Merufınıa E, Judı Sanı S, Nourı S (01 Mayıs 2015) Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi 36 3 2143–2152.
IEEE E. Merufınıa, S. Judı Sanı, ve S. Nourı, “Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model”, Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi, c. 36, sy. 3, ss. 2143–2152, 2015.
ISNAD Merufınıa, Edris vd. “Evaluation of Hydrodynamic and Sediment Transport Equations and Parameter Sensitivity Analysis Using the SRH_2D Model”. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi 36/3 (Mayıs 2015), 2143-2152.
JAMA Merufınıa E, Judı Sanı S, Nourı S. Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi. 2015;36:2143–2152.
MLA Merufınıa, Edris vd. “Evaluation of Hydrodynamic and Sediment Transport Equations and Parameter Sensitivity Analysis Using the SRH_2D Model”. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi, c. 36, sy. 3, 2015, ss. 2143-52.
Vancouver Merufınıa E, Judı Sanı S, Nourı S. Evaluation of Hydrodynamic and Sediment Transport equations and Parameter Sensitivity Analysis Using the SRH_2D Model. Cumhuriyet Üniversitesi Fen Edebiyat Fakültesi Fen Bilimleri Dergisi. 2015;36(3):2143-52.