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Turbulence measurements in the bubbly flow region of hydraulic jumps

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TLDR
In this article, Chanson et al. measured the air-water turbulent integral time and length scales in a large-scale hydraulic jump and showed that the dimensionless integral turbulent length scale Lxz/d1 was closely related to the inflow depth.
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This article is published in Experimental Thermal and Fluid Science.The article was published on 2008-10-01 and is currently open access. It has received 69 citations till now. The article focuses on the topics: Turbulence & Hydraulic jump.

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Citations
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Journal ArticleDOI

Free-surface fluctuations and turbulence in hydraulic jumps

TL;DR: In this paper, the free-surface fluctuations and air-water properties of the hydraulic jump roller were investigated physically for relatively small Froude numbers (2.4 < Fr-1 < 5.1) and relatively large Reynolds numbers (6.6 x 10(4) < Re < 1.3x 10(5)).
Journal ArticleDOI

Experimental Study of Turbulent Fluctuations in Hydraulic Jumps

TL;DR: In this article, the free-surface and two-phase flow properties for a wide range of Froude numbers (3.8
Journal ArticleDOI

Convective transport of air bubbles in strong hydraulic jumps

TL;DR: In this paper, the convective transport of air bubbles in the jump roller is re-visited and some analytical extension is presented and the theoretical results are compared with some laboratory experiments conducted in a large-size facility operating at large Froude numbers.
Journal ArticleDOI

A Comprehensive Sub-Grid Air Entrainment Model for RaNS Modeling of Free-Surface Bubbly Flows

TL;DR: In this article, a sub-grid model was derived and implemented in a computational multiphase fluid dynamics (CMFD) framework to solve the Reynolds-averaged two-fluid equations.
Journal ArticleDOI

Air entrainment and turbulent fluctuations in hydraulic jumps

TL;DR: In this paper, a hydraulic jump is the sudden transition from a high-velocity impinging flow into a turbulent roller in an open channel, and significant free-surface fluctuations take place above the roller.
References
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BookDOI

Multiphase Flows with Droplets and Particles

TL;DR: In this article, the authors present a test case for a single-phase flow Turbulence Modulation by Particles (SPM) model using the Brownian Motion model.
Book

Open channel flow

TL;DR: The importance of basic principles is recognized in this article in two ways : first, by devoting the opening chapters to a fairly leisurely discussion of introductory principles, including a recapitulation of the underlying arguments derived from the parent subject of fluid mechanics; and second, by takingnevery opportunity in the later chapters to refer back to this earlier material in order to clarify particular applications as they arise.
Book

Air Bubble Entrainment in Free-Surface Turbulent Shear Flows

TL;DR: In this article, the authors investigated the air bubble entrainment in free-surface turbulent shear flows and developed an analysis of the air entraining processes in free surface flows.
Book

The Hydraulics of Open Channel Flow: An Introduction

TL;DR: In this paper, the authors present an introduction to the hydraulics of open channel flows and the application of the Bernoulli principle and Momentum equation to open channel flow calculations.

The Hydraulics of Open Channel Flow: An Introduction. Physical Modelling of Hydraulics

TL;DR: A physical model is a scaled representation of a hydraulic flow situation as discussed by the authors, which can help the decision-makers to visualize and to picture the flow field, before selecting a ''suitable'' design.
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Frequently Asked Questions (13)
Q1. What contributions have the authors mentioned in the paper "Turbulence measurements in the bubbly flow region of hydraulic jumps" ?

The measurements of interfacial velocity and turbulence level distributions provided new information on the turbulent velocity field in the highly-aerated shear region. The velocity profiles tended to follow a wall jet flow pattern. 

Once the entrained bubbles were advected into regions of lesser shear, bubble coalescence led to the formation of larger air bubbles which were driven by buoyancytowards the free-surface. 

In skimming flows, air bubble entrainment takes place in the form of some interfacial aeration, and the entrained bubbles are advected in a boundary layer flow. 

With any ultrasonic displacement meter, the signal output is a function of the strength of the acoustic signal reflected by the‘‘free-surface”. 

The ultrasonic displacement probes were calibrated with clearwater at rest against pointer gauge measurements for a range of water depths shortly before each experiment. 

The air–water flow properties were measured with either two single type conductivity probes (£ = 0.35 mm) or a double-tip conductivity probe (£ = 0.25 mm, Dx = 7.0 mm). 

These large fluctuations in free-surface elevations reflected the unsteady, dynamic nature of the hydraulic jump, caused possibly by the production, break up and pairing of macro-scale turbulent vortices in the developing shear layer. 

It is believed to derive from the high levels of turbulent shear stresses in the air–water shear layer that break up the entrained air bubbles into finer air entities. 

The experimental observations showed systematically that the maximum void fraction Cmax and maximum bubble count rate Fmax were functions of the inflow Froude number Fr1, of the inflow Reynolds number Re and of the streamwise position (x x1)/d1. 

When two probe sensors were simultaneously sampled, the signals were analysed in terms of the auto-correlation and cross-correlation functions Rxx and Rxz, respectively (Fig. 2). 

In the present study, the distributions of interfacial velocity showed a decreasing velocity with increasing distance from the invert, while the magnitude of the velocity decreased with increasing distance from the jump toe at a given elevation (Fig. 8A). 

In hydraulic jumps with partially-developed inflow conditions, the void fraction and bubble count rate profiles showed consistently two distinct regions: (a) the turbulent shear region and (b) the upper region (e.g. Figs. 5 and 6). 

Rxz ds ð5Þwhere s is the time lag, Rxx is the normalized auto-correlation function of the reference probe signal, and Rxz is the normalized cross-Fig.