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相关概念视频

Laminar and Turbulent Flow01:07

Laminar and Turbulent Flow

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...
Hydrostatic Pressure Force on a Curved Surface01:04

Hydrostatic Pressure Force on a Curved Surface

Hydrostatic pressure on curved surfaces is a fundamental concept in fluid mechanics with broad applications in the civil engineering field. When fluid is in contact with a curved surface, as in a reservoir, dam, or storage tank, it exerts pressure that varies in magnitude and direction along the curved surface. To assess the total hydrostatic force exerted by the fluid on a curved structure, engineers typically isolate the fluid volume adjacent to the surface and analyze the forces acting on...
Bernoulli's Equation for Flow Along a Streamline01:30

Bernoulli's Equation for Flow Along a Streamline

Bernoulli's equation relates the energy conservation in a fluid moving along a streamline. The equation applies to incompressible and inviscid fluids under steady flow. For such a flow, Newton's second law is applied to a small fluid element, which experiences forces due to pressure differences, gravity, and velocity variations. The force balance leads to the following form of Bernoulli's equation:
Bernoulli's Equation for Flow Normal to a Streamline01:16

Bernoulli's Equation for Flow Normal to a Streamline

Bernoulli's equation for flow normal to a streamline explains how pressure varies across curved streamlines due to the outward centrifugal forces induced by the fluid's curvature. The pressure is higher on the inner side of the curve, near the center of curvature, and decreases outward to balance these centrifugal forces.
The pressure difference depends on the fluid's velocity and radius of curvature. The pressure variation is minimal in flows with nearly straight streamlines. However, the...
Plane Potential Flows01:23

Plane Potential Flows

Plane potential flows simplify fluid motion by assuming the fluid to be irrotational and incompressible. These characteristics allow these flows to be described by a velocity potential function, ϕ, representing the flow speed in a given direction, and a stream function, ψ, that visualizes the flow path, both governed by Laplace's equation. These parameters help in estimating flow patterns, velocity distributions, and pressure fields around various hydraulic structures.
Uniform Flow
Uniform flow...
Design Example: Creating a Hydraulic Model of a Dam Spillway01:21

Design Example: Creating a Hydraulic Model of a Dam Spillway

Scaled hydraulic models of dam spillways provide a practical way to replicate and study the intricate flow dynamics of these structures. Often built to a 1:15 ratio, these models allow for observing critical water behavior, such as velocity distribution, flow patterns, and energy dissipation.

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相关实验视频

Updated: Jun 18, 2026

Experimental Investigation of Secondary Flow Structures Downstream of a Model Type IV Stent Failure in a 180° Curved Artery Test Section
11:00

Experimental Investigation of Secondary Flow Structures Downstream of a Model Type IV Stent Failure in a 180° Curved Artery Test Section

Published on: July 19, 2016

在劳背弧中,一个复杂的地幔流动模式.

G P Smith1, D A Wiens, K M Fischer

  • 1Department of Earth and Planetary Sciences, Washington University in St. Louis, 1 Brookings Drive, CB1169, St. Louis, MO 63130, USA.

Science (New York, N.Y.)
|April 28, 2001
PubMed
概括

剪波分裂揭示了加弧和劳盆地下方复杂的地幔流. 这种流动受到萨摩亚羽毛与太平洋板块相互作用的影响,而不仅仅是板块沉降.

科学领域:

  • 地质物理学 地质物理学
  • 地震学 地震学
  • 地幔动力学地幔动力学

背景情况:

  • 加弧和劳背弧中的亚齐穆斯特异性模式是复杂的.
  • 以前的模型很难解释这些模式,仅仅通过地幔流与太平洋板的下降相结合.

研究的目的:

  • 为了研究通加弧和劳回弧中复杂的亚齐木斯特异性.
  • 了解这个地区地幔流动背后的驱动力.

主要方法:

  • 对来自当地地震事件的剪切波分裂的分析.
  • 在陆地和海洋底部记录地震数据.
  • 与同位素数据的相关性.

主要成果:

  • 观测到复杂的亚齐木斯特异性,不由板合地幔流量解释.
  • 确定了地幔流动方向的旋转:汇聚-平行 (斐济),北-南 (劳盆地) 和弧-平行 (通加弧).
  • 同位素表明萨摩亚羽毛通过太平洋板块撕裂流入劳盆地.

结论:

  • 地幔在加弧和背弧下的流动是复杂的,并且受到超出简单板块沉降的因素的影响.
  • 萨摩亚羽毛在塑造劳盆地地幔动态方面发挥着重要作用.

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Visualization of Flow Field Around a Vibrating Pipeline Within an Equilibrium Scour Hole

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相关实验视频

Last Updated: Jun 18, 2026

Experimental Investigation of Secondary Flow Structures Downstream of a Model Type IV Stent Failure in a 180° Curved Artery Test Section
11:00

Experimental Investigation of Secondary Flow Structures Downstream of a Model Type IV Stent Failure in a 180° Curved Artery Test Section

Published on: July 19, 2016

Visualizing Hyporheic Flow Through Bedforms Using Dye Experiments and Simulation
09:49

Visualizing Hyporheic Flow Through Bedforms Using Dye Experiments and Simulation

Published on: November 18, 2015

Visualization of Flow Field Around a Vibrating Pipeline Within an Equilibrium Scour Hole
09:37

Visualization of Flow Field Around a Vibrating Pipeline Within an Equilibrium Scour Hole

Published on: August 26, 2019

  • 太平洋板块的裂促进了萨摩亚羽毛与主导板块的相互作用.