DNS-based characterization of pseudo-random roughness in minimal channels

TL;DR

This study uses direct numerical simulation to analyze turbulent flow over irregular rough surfaces in minimal channels, validating the approach and examining the influence of roughness characteristics on flow properties and surface forces.

Contribution

It demonstrates the effectiveness of minimal channel simulations for characterizing rough surfaces and explores the impact of roughness statistics on flow and force distributions.

Findings

Minimal channel approach accurately predicts roughness function and zero-plane displacement.

Surface force distribution exhibits anisotropic, spanwise-elongated structures.

Existing roughness correlations have limited predictive accuracy within ±30%.

Abstract

Direct numerical simulation is used to study turbulent flow over irregular rough surfaces in the periodic minimal channel configuration. The generation of irregular rough surface is based on a random algorithm, in which the power spectrum of the roughness height function along with its probability density function can be directly prescribed. The hydrodynamic properties of the roughness are investigated and compared to those obtained from full-size DNS for 12 roughness topographies with systematically varied PDF and PS at four roughness height. The comparison confirms the viability of the minimal channel approach for characterization of rough surfaces providing excellent agreement in roughness function and zero-plane displacement across various types of roughness and different regimes. Results also indicates that different realizations of roughness, with a fixed PS and PDF, translate to similar values of roughness function with a small scatter. In addition to the global flow properties, the distribution of time-averaged surface force exerted by the roughness onto the fluid is examined and compared to the roughness height distribution for different cases. It is shown that the surface force distribution has an anisotropic structure with spanwise-elongated coherent regions. The anisotropy translates into a very small streamwise integral length scale, which weakly depends on the considered roughness topography, while the larger spanwise integral length scale shows a stronger dependence on roughness characteristics. It is also shown that the sheltering model describes well the spatial distribution of the surface force. Finally, existing roughness correlations are assessed using the present dataset. It was shown that the most correlations can reproduce the values of equivalent sand-grain roughness from DNS within+-30% error while none of the correlations shows a superior predictive accuracy.