Download An introduction to computational fluid dynamics by H. Versteeg, W. Malalasekera PDF

By H. Versteeg, W. Malalasekera

This proven, top textbook, is acceptable for classes in CFD. the recent variation covers new thoughts and techniques, in addition to huge enlargement of the complex subject matters and functions (from one to 4 chapters).


This ebook provides the basics of computational fluid mechanics for the amateur person. It presents an intensive but hassle-free advent to the governing equations and boundary stipulations of viscous fluid flows, turbulence and its modelling, and the finite quantity approach to fixing stream difficulties on computers.


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Extra resources for An introduction to computational fluid dynamics

Sample text

The final result is that the discontinuity remains undiminished due to the absence of a dissipation mechanism to remove the kink in the slope. Compressible fluid flows at speeds close to and above the speed of sound exhibit shockwaves and it turns out that the inviscid flow equations are hyperbolic at these speeds. The shockwave discontinuities are manifestations of the hyperbolic nature of such flows. Computational algorithms for hyperbolic problems are shaped by the need to allow for the possible existence of discontinuities in the interior of the solution.

Even in flows where the mean velocities and pressures vary in only one or two space dimensions, turbulent fluctuations always have a threedimensional spatial character. Furthermore, visualisations of turbulent flows reveal rotational flow structures, so-called turbulent eddies, with a wide range of length scales. 2, which depicts a cross-sectional view of a turbulent boundary layer on a flat plate, shows eddies whose length scale is comparable with that of the flow boundaries as well as eddies of intermediate and small size.

At these speeds the Reynolds number is usually very high and the viscous regions in the flow are usually very thin. The flow in a large part of the solution region behaves as an effectively inviscid fluid. This gives rise to problems in external flows, because the part of the flow where the outer boundary conditions are applied behaves in an inviscid way, which differs from the (viscous) region of flow on which the overall classification is based. 4) needs to be modified. The transient version of the algorithm needs to be adopted to make use of the favourable character of parabolic/hyperbolic procedures.

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