# Direct numerical simulations of Taylor--Couette turbulence: the effect   of sand grain roughness

**Authors:** Pieter Berghout, Xiaojue Zhu, Daniel Chung, Roberto Verzicco, Richard, J.A.M. Stevens, Detlef Lohse

arXiv: 1812.02265 · 2021-01-20

## TL;DR

This study uses direct numerical simulations to investigate how sand grain roughness affects turbulence in Taylor--Couette flow, revealing that roughness causes a downward shift in the logarithmic layer similar to pipe flow, across a range of flow conditions.

## Contribution

The paper introduces an improved simulation model for monodisperse sand grain roughness in Taylor--Couette flow and analyzes its impact on turbulence and skin-friction drag.

## Key findings

- Roughness causes a downward shift in the logarithmic layer.
- Shift behavior is similar to that observed in pipe flow.
- Effect consistent across different Taylor numbers.

## Abstract

Progress in roughness research, mapping any given roughness geometry to its fluid dynamic behaviour, has been hampered by the lack of accurate and direct measurements of skin-friction drag, especially in open systems. The Taylor--Couette (TC) system has the benefit of being a closed system, but its potential for characterizing irregular, realistic, 3-D roughness has not been previously considered in depth. Here, we present direct numerical simulations (DNSs) of TC turbulence with sand grain roughness mounted on the inner cylinder. The model proposed by Scotti (\textit{Phys. Fluids}, vol. 18, 031701, 2006) has been improved to simulate a random rough surface of monodisperse sand grains, which is characterized by the equivalent sand grain height $k_s$. Taylor numbers range from $Ta = 1.0\times 10^7$(corresponding to $Re_\tau = 82$) to $Ta = 1.0\times 10^9$($Re_\tau = 635$). We focus on the influence of the roughness height $k_s^+$ in the transitionally rough regime, through simulations of TC with rough surfaces, ranging from $k_s^+=5$ up to $k_s^+ = 92$, where the superscript `$+$' indicates non-dimensionalization in viscous units. We find that the downwards shift of the logarithmic layer, due to transitionally rough sand grains exhibits remarkably similar behavior to that of the Nikuradse (\textit{VDI-Forschungsheft} 361, 1933) data of sand grain roughness in pipe flow, regardless of the Taylor number dependent constants of the logarithmic layer.

## Full text

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## Figures

37 figures with captions in the complete paper: https://tomesphere.com/paper/1812.02265/full.md

## References

48 references — full list in the complete paper: https://tomesphere.com/paper/1812.02265/full.md

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Source: https://tomesphere.com/paper/1812.02265