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関連する概念動画

Viscosity of Fluid01:19

Viscosity of Fluid

2.2K
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.
2.2K
Viscosity01:17

Viscosity

7.9K
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...
7.9K
Viscosity01:27

Viscosity

113
Viscosity is a property of fluids that measures their resistance to flow. It is influenced by factors such as the surface area of contact, the gradient of flow speed, and the fluid's viscosity constant, called the coefficient of viscosity. The coefficient of viscosity, also known as dynamic viscosity, is denoted by the symbol η. It determines the proportionality between the viscous force and the gradient of flow speed.Newton's law of viscosity states that the viscous force on a...
113
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

1.8K
An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
1.8K
Magnetic Susceptibility and Permeability01:31

Magnetic Susceptibility and Permeability

2.7K
In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
2.7K
Surface Tension, Capillary Action, and Viscosity02:57

Surface Tension, Capillary Action, and Viscosity

34.5K
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...
34.5K

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関連する実験動画

Updated: Mar 28, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

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地球のマントルの真ん中の粘度ジャンプ

Maxwell L Rudolph1, Vedran Lekić2, Carolina Lithgow-Bertelloni3

  • 1Department of Geology, Portland State University, Post Office Box 751, Portland, OR 97207, USA. maxwell.rudolph@pdx.edu.

Science (New York, N.Y.)
|December 15, 2015
PubMed
まとめ

科学者は800~1200kmの深さの 深いマントルの粘度が 大きく増加していることを発見しました この発見は 停滞した地形板や マントルの渦巻のような現象を 説明するのに役立ちます

科学分野:

  • 地理学
  • 地球科学
  • マントルダイナミクス

背景:

  • 深いマントルの粘度が地球の熱進化,羽根の動態,物質の混合に影響する.
  • マントルの層構造を理解することは,大規模な地質学的プロセスを理解するために不可欠です.

研究 の 目的:

  • 地球の深層マントルの粘性層を 推測する事になる
  • 粘度変化と観測された深層マントルの構造との関係を調査する.

主な方法:

  • 長波長非水静的ジオイドデータの再分析
  • 深さによる粘度変化を測定するための新しい方法を使用します.

主要な成果:

  • マントルの粘度が800~1200kmの深さで 大きく増加した.
  • この粘度上昇は,マントルの移行領域以下で起こります.
  • 粘度上昇の深さは,スラブの停滞と羽根の傾斜の地震観測と相関しています.

結論:

  • 推測された粘度増加は,観測された深層マントルの現象に統一的な説明を提供します.
  • この発見は,マントルの粘度層に関する以前の仮定に異議を唱える.

さらに関連する動画

Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package
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Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package

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Evolution of Staircase Structures in Diffusive Convection
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Evolution of Staircase Structures in Diffusive Convection

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関連する実験動画

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Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

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Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package
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Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package

Published on: September 17, 2021

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Evolution of Staircase Structures in Diffusive Convection
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Evolution of Staircase Structures in Diffusive Convection

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  • 深いマントルの動態における粘度構造の重要性を強調する.