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相关概念视频

Turbulent Flow01:24

Turbulent Flow

186
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...
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Laminar and Turbulent Flow01:07

Laminar and Turbulent Flow

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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...
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Reynolds Transport Theorem01:24

Reynolds Transport Theorem

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The Reynolds transport theorem provides a framework to relate the time rate of change of an extensive property within a system to that in a control volume, which is crucial for analyzing fluid dynamics. Extensive properties, such as mass, velocity, acceleration, temperature, and momentum, can be expressed in terms of the mass of a fluid portion. These properties are called extensive because they depend on the system's size, while intensive properties are their corresponding values per unit...
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Boundary Layer Characteristics01:18

Boundary Layer Characteristics

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When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
109
Viscosity01:17

Viscosity

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When water is poured into a glass, it falls freely and quickly, whereas if honey or maple syrup is poured over a pancake, it flows slowly and sticks to the surface of the container. This difference in the flow of different kinds of liquids arises due to the fluid friction between the liquid layers and the liquid and the surrounding material. This property of fluids is called fluid viscosity. In this example, water has a lower viscosity than honey and maple syrup.
The SI unit of viscosity is...
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Poiseuille's Law and Reynolds Number01:10

Poiseuille's Law and Reynolds Number

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Any fluid in a horizontal tube can flow due to pressure differences—fluid flows from high to low pressure. The flow rate (Q) is the ratio of pressure difference and resistance through a horizontal tube. The greater the pressure difference, the higher the flow rate. The flow resistance is expressed as:
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相关实验视频

Updated: Jul 1, 2025

Visually Based Characterization of the Incipient Particle Motion in Regular Substrates: From Laminar to Turbulent Conditions
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Visually Based Characterization of the Incipient Particle Motion in Regular Substrates: From Laminar to Turbulent Conditions

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动荡运输中的棘手问题

Antonio Celani1, Gautam Reddy2,3,4, Massimo Vergassola5,6

  • 1The Abdus Salam International Centre for Theoretical Physics (ICTP), Strada Costiera 11, I-34014 - Trieste, Italy.

Annales Henri Poincare
|March 1, 2024
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概括
此摘要是机器生成的。

这项研究探讨了流运输中的粒子粘性. 我们发现,部分粘度会影响运输动态,并为大气模型引入新的边界条件.

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The Diffusion of Passive Tracers in Laminar Shear Flow
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The Diffusion of Passive Tracers in Laminar Shear Flow
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科学领域:

  • 物理 物理学 物理
  • 流体动力学 流体动力学
  • 大气科学 大气科学

背景情况:

  • 流运输在各种科学领域至关重要.
  • 粒子-表面相互作用可以显著改变运输现象.
  • 现有的模型可能无法完全捕捉部分粘度的细微差别.

研究的目的:

  • 为了研究部分颗粒粘度对流运输的影响.
  • 用一种新方法重新推导可压缩克赖南模型的已知结果.
  • 开发和分析一种新的大气边界层运输模型,考虑粘性.

主要方法:

  • 利用双直角性方法,以左和右自向量来扩展传播器.
  • 应用直角性和规范化约束来重新推导现有结果.
  • 引入了大气边界层的通用运输模型,其高度依赖的漂移和扩散性.

主要成果:

  • 为可压缩的克赖南模型重新衍生出已知的结果,证实了双正交法方法的有效性.
  • 在粒子与表面相互作用强度 (V) 介于 -1 到 1 (不包括 0) 之间时,确定了大气传输的允许边界条件的一个参数家族.
  • 确定了该范围以外的V的单一允许边界条件,与完全粘附或没有粘附相关.

结论:

  • 双直角性方法提供了一种直观的方法来理解带有部分粘度的流运输.
  • 粒子与地面的粘附程度是大气边界层运输中的一个关键参数.
  • 这些发现提供了更精细的了解在大气中的标记物运输.