Invariant p.d.f. property of velocity fluctuation in high-Reynolds-number turbulent boundary layer

Streamwise velocity fluctuations are measured in a zero-pressure gradient turbulent boundary layer at high Reynolds numbers. When normalised by the mean and standard deviation, u Subscript r <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>u</mml:mi> <mml:mi>r</mml:mi> </mml:msub> </mml:math> $u_r$ , the probability density function (p.d.f.) of the fluctuations exhibits invariance within distinct wall-normal regions. Two such regions were identified: one situated near the plateau of the turbulence intensity profile and the other associated with the logarithmic region ( left parenthesis u Subscript r Superscript plus Baseline right parenthesis squared equals upper A 1 ln left parenthesis y divided by delta right parenthesis plus upper B 1 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:mo stretchy="false">(</mml:mo> <mml:msubsup> <mml:mi>u</mml:mi> <mml:mi>r</mml:mi> <mml:mo>+</mml:mo> </mml:msubsup> <mml:msup> <mml:mo stretchy="false">)</mml:mo> <mml:mn>2</mml:mn> </mml:msup> <mml:mo>=</mml:mo> <mml:msub> <mml:mi>A</mml:mi> <mml:mn>1</mml:mn> </mml:msub> <mml:mi>ln</mml:mi> <mml:mo>⁡</mml:mo> <mml:mo stretchy="false">(</mml:mo> <mml:mi>y</mml:mi> <mml:mrow> <mml:mo>/</mml:mo> </mml:mrow> <mml:mi>δ</mml:mi> <mml:mo stretchy="false">)</mml:mo> <mml:mo>+</mml:mo> <mml:msub> <mml:mi>B</mml:mi> <mml:mn>1</mml:mn> </mml:msub> </mml:math> $(u_r^+)^2=A_1 \ln (y/\delta )+B_1$ ) consistent with Townsend’s attached-eddy hypothesis. The p.d.f. shapes in both regions are independent of Reynolds number, demonstrating their universality. The slope, upper A 1 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>A</mml:mi> <mml:mn>1</mml:mn> </mml:msub> </mml:math> $A_1$ , and additive constant, upper B 1 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>B</mml:mi> <mml:mn>1</mml:mn> </mml:msub> </mml:math> $B_1$ , were evaluated to be upper A 1 asymptotically equals 1.42 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>A</mml:mi> <mml:mn>1</mml:mn> </mml:msub> <mml:mo>≃</mml:mo> <mml:mn>1.42</mml:mn> </mml:math> $A_1 \simeq 1.42$ and upper B 1 asymptotically equals 1.75 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>B</mml:mi> <mml:mn>1</mml:mn> </mml:msub> <mml:mo>≃</mml:mo> <mml:mn>1.75</mml:mn> </mml:math> $B_1 \simeq 1.75$ , respectively, for upper O left parenthesis 10 Superscript 4 Baseline right parenthesis less than italic Re Subscript tau <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:mi>O</mml:mi>

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Journal
Journal of Fluid Mechanics
Published
2026-06-18
DOI
https://doi.org/10.1017/jfm.2026.11568
Primary Topic
Fluid Dynamics and Turbulent Flows
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article
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article

Invariant p.d.f. property of velocity fluctuation in high-Reynolds-number turbulent boundary layer

Yoshiyuki Tsuji, Atsushi IDO
Journal of Fluid Mechanics
Fluid Dynamics and Turbulent Flows
article

Invariant p.d.f. property of velocity fluctuation in high-Reynolds-number turbulent boundary layer

Yoshiyuki Tsuji, Atsushi IDO
article en

Abstract

Streamwise velocity fluctuations are measured in a zero-pressure gradient turbulent boundary layer at high Reynolds numbers. When normalised by the mean and standard deviation, u Subscript r <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>u</mml:mi> <mml:mi>r</mml:mi> </mml:msub> </mml:math> $u_r$ , the probability density function (p.d.f.) of the fluctuations exhibits invariance within distinct wall-normal regions. Two such regions were identified: one situated near the plateau of the turbulence intensity profile and the other associated with the logarithmic region ( left parenthesis u Subscript r Superscript plus Baseline right parenthesis squared equals upper A 1 ln left parenthesis y divided by delta right parenthesis plus upper B 1 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:mo stretchy="false">(</mml:mo> <mml:msubsup> <mml:mi>u</mml:mi> <mml:mi>r</mml:mi> <mml:mo>+</mml:mo> </mml:msubsup> <mml:msup> <mml:mo stretchy="false">)</mml:mo> <mml:mn>2</mml:mn> </mml:msup> <mml:mo>=</mml:mo> <mml:msub> <mml:mi>A</mml:mi> <mml:mn>1</mml:mn> </mml:msub> <mml:mi>ln</mml:mi> <mml:mo>⁡</mml:mo> <mml:mo stretchy="false">(</mml:mo> <mml:mi>y</mml:mi> <mml:mrow> <mml:mo>/</mml:mo> </mml:mrow> <mml:mi>δ</mml:mi> <mml:mo stretchy="false">)</mml:mo> <mml:mo>+</mml:mo> <mml:msub> <mml:mi>B</mml:mi> <mml:mn>1</mml:mn> </mml:msub> </mml:math> $(u_r^+)^2=A_1 \ln (y/\delta )+B_1$ ) consistent with Townsend’s attached-eddy hypothesis. The p.d.f. shapes in both regions are independent of Reynolds number, demonstrating their universality. The slope, upper A 1 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>A</mml:mi> <mml:mn>1</mml:mn> </mml:msub> </mml:math> $A_1$ , and additive constant, upper B 1 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>B</mml:mi> <mml:mn>1</mml:mn> </mml:msub> </mml:math> $B_1$ , were evaluated to be upper A 1 asymptotically equals 1.42 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>A</mml:mi> <mml:mn>1</mml:mn> </mml:msub> <mml:mo>≃</mml:mo> <mml:mn>1.42</mml:mn> </mml:math> $A_1 \simeq 1.42$ and upper B 1 asymptotically equals 1.75 <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:msub> <mml:mi>B</mml:mi> <mml:mn>1</mml:mn> </mml:msub> <mml:mo>≃</mml:mo> <mml:mn>1.75</mml:mn> </mml:math> $B_1 \simeq 1.75$ , respectively, for upper O left parenthesis 10 Superscript 4 Baseline right parenthesis less than italic Re Subscript tau <mml:math xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mnf="http://cambridge.org/core/manifest" xmlns:cup="http://contentservices.cambridge.org" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:m="http://cambridge.org/core/metadata" xmlns:core="http://cambridge.org/core" xmlns:c="http://cambridge.org/core/content"> <mml:mi>O</mml:mi>

Journal of Fluid MechanicsVol. 1037
Shanghai Tunnel Engineering (China) (CN), German Dutch Wind Tunnels (NL), Nagoya University (JP)
Openalex Percentile: Top 6%
Fluid Dynamics and Turbulent Flows
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