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Turbulent Flow01:24

Turbulent Flow

Turbulent flow is characterized by unpredictable fluctuations in velocity and pressure, which result in a chaotic fluid movement distinct from the orderly patterns of laminar flow. While laminar flow is governed by smooth, parallel layers with minimal mixing, turbulent flow exhibits highly irregular, three-dimensional patterns. This behavior arises due to instabilities in the fluid's velocity profile, and amplifies as the flow velocity increases. Minor disturbances, known as turbulent spots,...
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Fluid mechanics model studies often utilize scaled-down systems to predict fluid behavior in full-scale environments, such as river flows, dam spillways, and structures interacting with open surfaces. Maintaining Froude number similarity in river models is crucial, as it replicates surface flow features like wave patterns and velocities.
Laminar and Turbulent Flow01:07

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Fluid dynamics is the study of fluids in motion. Velocity vectors are often used to illustrate fluid motion in applications like meteorology. For example, wind—the fluid motion of air in the atmosphere—can be represented by vectors indicating the speed and direction of the wind at any given point on a map. Another method for representing fluid motion is a streamline. A streamline represents the path of a small volume of fluid as it flows. When the flow pattern changes with time, the streamlines...
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Fluid flows are categorized by dimensionality and behavior, with one-dimensional flow being the simplest form, where properties like velocity and pressure change only along a single axis. Water moving through straight pipes exemplifies this flow type, as variations in other directions are minimal. One-dimensional analysis helps simplify understanding such flows, focusing solely on changes along the pipe's length.
Two-dimensional flow involves changes in both length and height, as seen in air...
Rapidly Varying Flow01:24

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Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
Weir: Problem Solving01:26

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Water flow in open channels is often measured using hydraulic structures such as weirs, which allow precise calculation of discharge. In a rectangular channel, flow rates are measured using three types of weirs: rectangular sharp-crested, triangular sharp-crested, and broad-crested. The weir head is set at a fixed height above the channel bottom, simplifying calculations and enabling the relationship between depth and flow rate to be analyzed.For the rectangular sharp-crested weir, the flow...

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Related Experiment Video

Updated: May 26, 2026

Preparation of Free-Surface Hyperbolic Water Vortices
04:35

Preparation of Free-Surface Hyperbolic Water Vortices

Published on: July 28, 2023

Different regimes for water wave turbulence.

P Cobelli1, A Przadka, P Petitjeans

  • 1Physique et Mécanique des Milieux Hétérogènes PMMH, UMR CNRS ESPCI-UPMC Univ. Paris, France.

Physical Review Letters
|December 21, 2011
PubMed
Summary

This study investigates gravity capillary wave turbulence, revealing that the wave spectrum can be forcing independent, aligning with theoretical predictions. This finding advances our understanding of complex wave dynamics.

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Area of Science:

  • Fluid Dynamics
  • Wave Turbulence Theory
  • Nonlinear Physics

Background:

  • Wave turbulence describes systems with a large number of weakly interacting waves.
  • Gravity capillary waves are surface waves influenced by both gravity and surface tension.
  • Understanding energy transfer in wave turbulence is crucial for various physical phenomena.

Purpose of the Study:

  • To experimentally investigate gravity capillary wave turbulence in water.
  • To analyze the behavior of wave energy density in 3D (k,ω) space.
  • To determine the dependence of the gravity spectral slope on forcing parameters.

Main Methods:

  • Utilized space-time resolved Fourier transform profilometry for precise measurements.
  • Examined wave energy density |η(k,ω)|² across different forcing frequency bandwidths and amplitudes.
  • Conducted experiments in a controlled water environment.

Main Results:

  • Observed two distinct behaviors for the gravity spectral slope based on bandwidth.
  • Identified a forcing-independent spectral slope under specific bandwidth conditions.
  • Demonstrated consistency between experimental results and the Zakharov-Filonenko cascade theory.

Conclusions:

  • The study confirms the existence of forcing-independent gravity spectral slopes in wave turbulence.
  • Experimental findings support the theoretical predictions of the Zakharov-Filonenko cascade.
  • Provides valuable insights into the fundamental mechanisms governing gravity capillary wave turbulence.