Abstract

Highly turbulent Taylor–Couette flow with spanwise-varying roughness is investigated experimentally and numerically (direct numerical simulations with an immersed boundary method) to determine the effects of the spacing and spanwise width ss of the spanwise-varying roughness on the total drag and on the flow structures. We apply sandgrain roughness, in the form of alternating rough and smooth bands to the inner cylinder. Numerically, the Taylor number is O(109)O(109) and the roughness width is varied in the range 0.47⩽s~=s/d⩽1.230.47⩽s~=s/d⩽1.23 , where dd is the gap width. Experimentally, we explore Ta=O(1012)Ta=O(1012) and 0.61⩽s~⩽3.740.61⩽s~⩽3.74 . For both approaches the radius ratio is fixed at η=ri/ro=0.716𝜂=ri/ro=0.716 , with riri and roro the radius of the inner and outer cylinder respectively. We present how the global transport properties and the local flow structures depend on the boundary conditions set by the roughness spacing s~s~ . Both numerically and experimentally, we find a maximum in the angular momentum transport as a function of s~s~ . This can be attributed to the re-arrangement of the large-scale structures triggered by the presence of the rough stripes, leading to correspondingly large-scale turbulent vortices.

Highlights

  • In most industrial applications and geophysical flows, turbulence is partly or completely wall bounded

  • We have investigated, both numerically and experimentally, large Taylor number Taylor–Couette flow in the presence of spanwise-varying roughness, which consists of an arrangement of stripes of width s, that covers the entire circumference of the inner cylinder

  • The stripes were made from sandpaper, while in the numerics a confocal microscopy scan of the surface was implemented by means of the immersed boundary method

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Summary

Introduction

In most industrial applications and geophysical flows, turbulence is partly or completely wall bounded. Boundaries are not smooth but their surface is rather irregular and rough Such flows are extensively studied, mainly under the approximation that the roughness is homogeneous (Jiménez 2004). Flows are bounded by rough boundaries that vary on the scale of k, and on a much larger scale s, with s = O(δ) Whereas these variations can occur either laterally (spanwise) or longitudinally (streamwise), we focus here only on the former. Such examples are found in shipping (i.e. the formation of stripes of bio-fouling on ship hulls (Schultz 2007)) and geophysical flows (e.g. the atmospheric flows over a spanwise-varying terrain (Ren & Wu 2011))

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