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相关概念视频

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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Irrotational Flow01:28

Irrotational Flow

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Irrotational flow is characterized by fluid motion where particles do not rotate around their axes, resulting in zero vorticity. For a flow to be irrotational, the curl of the velocity field must be zero. This imposes specific conditions on velocity gradients. For instance, to maintain zero rotation about the z-axis, the gradient condition:
404
Viscosity of Fluid01:19

Viscosity of Fluid

331
Viscosity measures the resistance a fluid offers to flow and deformation. It results from internal friction between layers of fluid moving relative to one another. Dynamic viscosity, denoted by the Greek letter mu (μ), quantifies the force needed to move one fluid layer over another. For Newtonian fluids like water and air, the relationship between the shearing stress and the rate of shearing strain is linear, meaning their viscosity remains constant regardless of the applied stress.
331
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...
8.4K
Surface Tension, Capillary Action, and Viscosity02:57

Surface Tension, Capillary Action, and Viscosity

27.5K
Surface Tension
The various IMFs between identical molecules of a substance are examples of cohesive forces. The molecules within a liquid are surrounded by other molecules and are attracted equally in all directions by the cohesive forces within the liquid. However, the molecules on the surface of a liquid are attracted only by about one-half as many molecules. Because of the unbalanced molecular attractions on the surface molecules, liquids contract to form a shape that minimizes the number...
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Steady, Laminar Flow Between Parallel Plates01:17

Steady, Laminar Flow Between Parallel Plates

130
Understanding steady, laminar flow between parallel plates is essential for analyzing and designing flow in narrow rectangular channels, commonly found in various water conveyance and drainage systems. The Navier-Stokes equations govern fluid motion and are generally challenging to solve due to their nonlinearity. However, simplifications are possible in certain cases, like the steady laminar flow between parallel plates. For this scenario, we assume steady, incompressible, laminar flow.
130

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相关实验视频

Updated: Jun 3, 2025

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
08:16

Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine

Published on: March 13, 2017

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温带冰的线性粘性流

Collin M Schohn1, Neal R Iverson1, Lucas K Zoet2

  • 1Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA, USA.

Science (New York, N.Y.)
|January 9, 2025
PubMed
概括

温带冰川表现为线性粘性物质,而不是以前所认为的非线性. 基于剪切变形实验的这一发现影响了海平面上升的预测.

科学领域:

  • 冰川学
  • 冰的物理
  • 气候科学

背景情况:

  • 对于预测海平面上升至关重要.
  • 目前的模型通常依赖于格伦的流量定律,假设非线性冰粘度 (n=3-4).
  • 温的冰在粒边上含有液态水,影响其机械行为.

研究的目的:

  • 在现实的压力和水分含量条件下研究温带冰川的浮动行为.
  • 为了确定温带冰变形的应变速率指数 (n).
  • 评估观察到的冰粘度对冰盖建模的影响.

主要方法:

  • 在温带冰川上进行大规模的剪切变形实验.
  • 冰川床和冰流边缘相关的范围内的液态水含量和应力.
  • 分析了应力和应变率之间的关系以确定粘度指数 (n).

主要成果:

  • 在测试条件下,温带冰川表现出线性粘性行为 (n ≈1.0).
  • 这与格伦的流量定律所假定的非线性粘度 (n=3-4) 形成鲜明对比.
  • 观察到的线性归因于在谷物边界的扩散压力化和重新结.

结论:

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  • 温带冰的线性粘性挑战了现有的冰流模型.
  • 这一发现可能有助于稳定冰盖应对气候变化的预测.
  • 修订后的模型包含了线性粘度,可以改善海平面上升的预测.