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Hydraulic Modeling Development and Application in Water Resources Engineering

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Part of the book series: Handbook of Environmental Engineering ((HEE,volume 14))

Abstract

The use of modeling has become widespread in water resources engineering and science to study rivers, lakes, estuaries, and coastal regions. For example, computer models are commonly used to forecast anthropogenic effects on the environment, and to help provide advanced mitigation measures against catastrophic events such as natural and dam-break floods. Linking hydraulic models to vegetation and habitat models has expanded their use in multidisciplinary applications to the riparian corridor. Implementation of these models in software packages on personal desktop computers has made them accessible to the general engineering community, and their use has been popularized by the need of minimal training due to intuitive graphical user interface front ends. Models are, however, complex and nontrivial, to the extent that even common terminology is sometimes ambiguous and often applied incorrectly. In fact, many efforts are currently under way in order to standardize terminology and offer guidelines for good practice, but none has yet reached unanimous acceptance. This chapter provides a view of the elements involved in modeling surface flows for the application in environmental water resources engineering. It presents the concepts and steps necessary for rational model development and use by starting with the exploration of the ideas involved in defining a model. Tangible form of those ideas is provided by the development of a mathematical and corresponding numerical hydraulic model, which is given with a substantial amount of detail. The issues of model deployment in a practical and productive work environment are also addressed. The chapter ends by presenting a few model applications highlighting the need for good quality control in model validation.

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Notes

  1. 1.

    The independent variables are the inputs and the forcing quantities, such as boundary conditions and spatial coordinates; the dependent variables are the outputs and effects, such as flow velocity and water surface elevation.

References

  1. 1. Kirby, M. J. (1987). Models in physical geography. In M. Clark et al. (Eds.), Horizons in physical geography. (pp. 47–61). Totowa: Barnes and Noble.

    Google Scholar 

  2. Bird, R., Stewart, W., & Lightfoot, E. (1960). Transport phenomena. New York: Wiley.

    Google Scholar 

  3. Formentin, S., & Zanuttigh, B. (2013). Prediction of wave transmission through a new artificial neural network developed for wave reflection. Proceedings of the 7th International Conference on Coastal Dynamics, Arcachon, France, 24–28 June 2013, pp. 627–638.

    Google Scholar 

  4. Azamathulla, H., & Zahiri, A. (2012). Flow discharge prediction in compound channels using linear genetic programming. Journal of Hydrology, 454–455, 203–207.

    Article  Google Scholar 

  5. Biswas, G. (2013). Computational fluid dynamics. Pangbourne: Alpha Science.

    Google Scholar 

  6. Rosenquist, T., & Story, S. (2012). Using the Intel Math Kernel Library (Intel MKL) and Intel compilers to obtain run-to-run numerical reproducible results. The Parallel Universe, no. 11, September 2012, pp. 26–28 Intel Corporation.

    Google Scholar 

  7. Refsgaard, J., & Henriksen, H. (2004). Modeling guidelines—terminology and guiding principles. Advances in Water Resources, 27, 71–82.

    Article  Google Scholar 

  8. EPA. (2009). Guidance on the development, evaluation, and application of environmental models. U.S. Environmental Protection Agency, Council for Regulatory Environmental Modeling, EPA/100/K-09/003, March 2009.

    Google Scholar 

  9. Tennekes, H., & Lumley, J. (1972). A first course in turbulence. Cambridge: MIT Press.

    Google Scholar 

  10. Rodi, W. (1993). Turbulence models and their application in hydraulics. IAHR monograph. Roterdam: Balkema.

    Google Scholar 

  11. Pritchard, D. W. (1971). Hydrodynamic models. Estuarine models: An assessment (pp. 33). Tracor, Inc, for the Water Quality Office of the Environmental Protection Agency.

    Google Scholar 

  12. Shimizu, Y., Yamaguchi, H., & Itakura, T. (1991). Three-dimensional computation of flow and bed deformation. Journal of Hydraulic Engineering, 116(9), 1090–1108.

    Article  Google Scholar 

  13. Vreugdenhil, C. (1994). Numerical methods for shallow-water flow. Boston: Kluwer.

    Google Scholar 

  14. Fischer, H. B., List, E. J., Koh, R. C. Y., Imberger, J., & Brooks, N. H. (1979). Mixing in inland and coastal waters. San Diego: Academic.

    Google Scholar 

  15. Roe, P. L. (1981). Approximate Riemann solvers, parameter vectors, and difference schemes. Journal of Computational Physics, 43, 357–372.

    Article  Google Scholar 

  16. Toro, E. F. (2001). Shock-capturing methods for free-surface shallow flows. Chichester: Wiley.

    Google Scholar 

  17. Alcrudo, F., & Garcia-Navarro, P. (1993). A high-resolution Godunov-type scheme in finite volumes in 2D shallow water equations. International Journal for Numerical Methods in Fluids, 16, 489–505.

    Article  CAS  Google Scholar 

  18. Harten, A., & Hyman, J. M. (1983). Self adjusting grid methods for one-dimensional hyperbolic conservation laws. Journal of Computational Physics, 50, 235–269.

    Article  Google Scholar 

  19. van Leer, B. (1979). Towards the ultimate conservative difference scheme, V. A second order sequel to Godunovʼs method. Journal of Computational Physics, 32, 101–136.

    Article  Google Scholar 

  20. Barth, T. J., & Jespersen, D. C. (1989). The design and application of upwind schemes on unstructured meshes. AIAA paper AIAA-89-0366.

    Google Scholar 

  21. Venkatakrishnan, V. (1995). Convergence to steady state solutions of the Euler equations on unstructured grids with limiters. Journal of Computational Physics, 118, 120–130.

    Article  Google Scholar 

  22. Rausch, R., Batina, J., & Yang, H. (1991). Spatial adaptation procedures on unstructured meshes for accurate unsteady aerodynamic flow computation. AIAA Paper 91-1106.

    Google Scholar 

  23. Batten, P., Lambert, C., & Causon, D. M. (1996). Positively conservative high-resolution convective schemes for unstructured elements. International Journal for Numerical Methods in Engineering, 39, 1821–1838.

    Article  Google Scholar 

  24. Coirier, W. J. (1994). An adaptively-refined, Cartesian, cell-based scheme for the Euler and Navier-Stokes equations, Ph.D. dissertation, Dept. of Aerospace Engineering, Univeristy of Michigan, MI.

    Google Scholar 

  25. Bradford, S. F., & Sanders, B. F. (2002). Finite-volume method for shallow water flooding of arbitrary topography. Journal of Hydraulic Engineering. ASCE, 128(3), 289–298.

    Article  Google Scholar 

  26. Gottlieb, S., Shu, C.-W., & Tadmor, E. (2001). Strong stability-preserving high-order time discretization methods. SIAM Review, 43(1), 89–112.

    Article  Google Scholar 

  27. Swanson, R. C., & Turkel, E. (1997). Multistage schemes with multigrid for Euler and Navier-Stokes equations, components and analysis. NASA technical paper 3631, Langley Research Center, Hampton, VA.

    Google Scholar 

  28. Jameson, A., & Mavriplis, D. (1986). Finite volume solution of the two-dimensional Euler equations on a regular triangular mesh. AIAA Journal, 24(4), 611–618.

    Article  Google Scholar 

  29. Horritt, M. S. (2002). Evaluating wetting and drying algorithms for finite element models of shallow water flow. International Journal for Numerical Methods in Engineering, 55, 835–851.

    Article  Google Scholar 

  30. Balzano, A. (1998). Evaluation of methods for numerical simulation of wetting and drying of shallow water flow models. Coastal Engineering, 34, 83–107.

    Article  Google Scholar 

  31. Anastasiou, K., & Chan, C. T. (1997). Solution of the 2D shallow water equations using the finite volume method on unstructured triangular meshes. International Journal for Numerical Methods in Fluids, 24, 1225–1245.

    Article  Google Scholar 

  32. Löhner, R., & Galle, M. (2002). Minimization of indirect addressing for edge-based field solvers. Communications in Numerical Methods in Engineering, 18, 335–343.

    Article  Google Scholar 

  33. George, A., & Liu, J. (1981). Computer solution of large sparse positive definite systems. Computational mathematics. Englewood Cliffs: Prentice-Hall.

    Google Scholar 

  34. Dokken, T., Hagen, T. R., & Hjelmervik, J. M. (2007). An introduction to general purpose computing on programmable graphics hardware. In G. Hasle, et al. (Eds.), Geometric modeling, numerical simulation, and optimization: Industrial mathematics at SINTEF (pp. 123–161). Springer.

    Google Scholar 

  35. Tarpanelli, A., Brocca, L., Melone, F., & Moramarco, T. (2013). Hydraulic modelling calibration in small rivers by using coarse resolution synthetic aperture radar imagery. Hydrological Processes, 27, 1321–1330.

    Article  Google Scholar 

  36. Gallegos, H. A., Schubert, J. E., & Sanders, B. F. (2009). Two-dimensional, high-resolution modeling of urban dam-break flooding: A case study of Baldwin Hills, California. Advances in Water Resources, 32, 1323–1335.

    Article  Google Scholar 

  37. Hunter, N. M., Bates, P. D., Neelz, S., Pender, G., Villanueva, I., Wright, N. G., Liang, D., Falconer, R. A., Lin, B., Waller, S., Crossley, A. J., & Mason, D. C. (2008). Benchmarking 2D hydraulic models for urban flooding. Water Management, 161, 13–30.

    Google Scholar 

  38. Williams, R. D., Brasington, J., Vericat, D., & Hicks, D. M. (2014). Hyperscale terrain modelling of braided rivers: Fusing mobile terrestrial laser scanning and optical bathymetric mapping. Earth Surface Processes and Landforms, 39, 167–183.

    Article  Google Scholar 

  39. Oreskes, N., Shrader-Frechette, K., & Belitz, K. (1994). Verification, validation and confirmation of numerical models in the earth sciences. Science, 263(5147), 641–646.

    Article  CAS  Google Scholar 

  40. Cueto-Felgueroso, L., Colominas, I., Fe, J., Navarrina, F., & Casteleiro, M. (2006). High order finite volume schemes on unstructured grids using moving least squares reconstruction. Application to shallow water dynamics. International Journal for Numerical Methods in Engineering, 65(3), 295–331.

    Article  Google Scholar 

  41. Rajaratnman, N., & Nwachukwu, B. A. (1983). Flow near groin-like structures. Journal of Hydraulic Engineering. ASCE, 109(3), 463–480.

    Article  Google Scholar 

  42. Tingsanchali, T., & Maheswaran, S. (1990). 2-D depth-averaged flow near groyne. Journal of Hydraulic Engineering. ASCE, 166(1), 71–86.

    Article  Google Scholar 

  43. Wagner, C. R., & Muller, D. S. (2002). Use of velocity data to calibrate and validate two-dimensional hydrodynamic models. Proceedings of the Second Federal Interagency Hydrologic Modeling Conference, Las Vegas, NV, July 29–August 1, 2002.

    Google Scholar 

  44. ASCE (1998). River width adjustment. II: Modeling. Journal of Hydraulic Engineering. ASCE, 124(9), 903–917.

    Article  Google Scholar 

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Acknowledgments

The author is grateful to Chad Wagner, USGS, Louisville, KY, for kindly providing the bathymetry and experimental measurements used for the Olmsted Lock and Dam case, and for his assistance in data preparation and interpretation. The model developed and presented in this work (System for Transport and River Modeling, SToRM) was supported by the National Research Program of the US Geological Survey. The SToRM model and corresponding documentation are available for free download from the iRIC Project Web pages at http://i-ric.org/en/.

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Glossary

CFD

Short for computational fluid dynamics, it is a discipline that uses numerical methods and algorithms to solve fluid mechanics problems with computers.

CGNS

A standard for the storage and retrieval of digital data produced in CFD applications. It stands for CFD general notation system.

Computational cell

Each individual point, or volume, of the lattice (computational grid) transforming the continuous real-world domains into its discrete counterpart, suitable for numerical evaluation and implementation on digital computers.

Digital terrain model

Also called a digital elevation model (DEM), it is a 3D digital representation of a terrain’s surface.

Eddy viscosity

A method to model the transfer of momentum caused by turbulent eddies that is mathematically similar to momentum transfer due to molecular diffusion, and that consists in replacing the fluid viscosity ν by an effective turbulent viscosity, ν t , also called the eddy viscosity.

Froude number (Fr)

A dimensionless quantity defined as the ratio of a characteristic velocity to a gravitational wave velocity.

Godunov scheme

A conservative finite-volume numerical scheme used in the solution of partial differential equations, which solves exact or approximate Riemann problems at inter-cell boundaries.

Graphical user interface

Type of computer-user interface that allows the user to interact with a computer program using pointing hardware devices, graphical icons, and other visual indicators.

Hydrology

The study of flow of water over the Earth’s surface

k–ε model

A turbulence model based on solving two differential transport equations, one for the turbulent kinetic energy k and the other for the rate of turbulent dissipation ε.

Model

A idealized representation of a system.

MUSCL

Short for modified upwind scheme for conservation laws, it is a method to describe (reconstruct) the states of the variables in a computational cell based on the cell-averaged states (and their gradients) obtained in the previous time step.

Navier–Stokes equations

Partial differential equations arising from Newton’s second law (conservation of momentum) that describe the motion of fluids.

Runge–Kutta methods

A family of implicit and explicit iterative methods used in temporal discretization for the approximation of solutions of ordinary differential equations.

Supercritical flow

A flow whose velocity is larger than the wave velocity, therefore with Fr > 1.

TVD

Total variation diminishing (TVD) is a property of certain discretization schemes used to solve hyperbolic partial differential equations that do not increase the total variation of the solution from one time step to the next.

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Simões, F. (2015). Hydraulic Modeling Development and Application in Water Resources Engineering. In: Yang, C., Wang, L. (eds) Advances in Water Resources Engineering. Handbook of Environmental Engineering, vol 14. Springer, Cham. https://doi.org/10.1007/978-3-319-11023-3_6

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  • DOI: https://doi.org/10.1007/978-3-319-11023-3_6

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