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相关概念视频

Mechanisms of Heat Transfer I01:14

Mechanisms of Heat Transfer I

5.9K
Just as interesting as the effects of heat transfer on a system are the methods by which the heat transfer occur. Whenever there is a temperature difference, heat transfer occurs. It may occur rapidly, such as through a cooking pan, or slowly, such as through the walls of a picnic ice box. So many processes involve heat transfer that it is hard to imagine a situation where no heat transfer occurs. Yet, every heat transfer takes place by only three methods: conduction, convection, and radiation.
5.9K
Mechanisms of Heat Transfer II01:20

Mechanisms of Heat Transfer II

4.5K
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
4.5K
Isothermal Processes01:21

Isothermal Processes

3.8K
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
3.8K
Shearing Stress01:18

Shearing Stress

2.5K
Shearing stress, denoted by the Greek letter tau (τ), is stress caused by forces acting transversely on an object. These forces create internal ones within the entity in the plane where the external forces are applied. The resultant of these internal forces is the shear in the section.
The average shearing stress can be calculated by dividing the shear by the area of the cross-section.
2.5K
Elastic Strain Energy for Shearing Stresses01:20

Elastic Strain Energy for Shearing Stresses

682
As discussed in previous lessons, strain energy in a material is the energy stored when it is elastically deformed, a concept crucial in materials science and mechanical engineering. This energy results from the internal work done against the cohesive forces within the material. When a material undergoes shearing stress and corresponding shearing strain, the strain energy density, which is the energy stored per unit volume, is calculated. Within the elastic limit, where the stress is...
682
Mechanisms of Heat Transfer01:14

Mechanisms of Heat Transfer

1.9K
Heat transfer between the human body and its environment occurs through four main mechanisms: conduction, convection, radiation, and evaporation.
Conduction, accounting for approximately 3% of body heat loss at rest, is the process of exchanging heat between molecules of two materials in direct contact. This can result in both heat loss and gain. For instance, when the body is submerged in water, which conducts heat 20 times more effectively than air, it can either lose or gain significant...
1.9K

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相关实验视频

Updated: May 5, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

12.0K

在地幔中发生中等深度地震的周期性剪切加热机制.

Peter B Kelemen1, Greg Hirth

  • 1Department of Earth and Environmental Sciences, Columbia University, Lamont Doherty Earth Observatory, Palisades, New York 10964, USA. peterk@ldeo.columbia.edu

Nature
|April 13, 2007
PubMed
概括

中等深度地震源于局部粘性爬行,而不仅仅是脱水. 这种新模型解释了俯冲区以下的地震活动,揭示了准周期性的不稳定周期.

科学领域:

  • 地质物理学 地质物理学
  • 地震学 地震学
  • 构造学 构造学 构造学 构造学

背景情况:

  • 中等深度的地震发生在柔软-柔性过渡下方的俯冲区.
  • 现有的模型表明热或脱水机制,但这些对于一些地震地点是不够的.
  • 在这些深度的高压使得摩擦故障不太可能.

研究的目的:

  • 建议和建模用于中度深度地震的替代机制.
  • 为了解释发生在含水矿物质存在的深度以下的地震活动.

主要方法:

  • 在粗粒度弹性半空间内的细粒度剪切区域的数值建模.
  • 利用奥利文流动规律并模拟剪切加热效应.
  • 结合初始温度 (600-800°C) 和背景应变速率 (10−1210−15秒−1).

主要成果:

  • 由于剪切加热,局部粘性爬行迅速开始,增加了拉伸速率和温度.
  • 应变速率超过1s-1和温度达到1,400°C,然后是应力下降.
  • 这个过程导致在持续的远场变形下,半周期性的地震不稳定.

结论:

更多相关视频

High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus
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High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus

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Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System
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Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System

Published on: August 7, 2018

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相关实验视频

Last Updated: May 5, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
11:50

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

Published on: June 13, 2015

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High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus
12:30

High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus

Published on: April 3, 2018

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Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System
10:52

Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System

Published on: August 7, 2018

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  • 在细粒度剪切区域的粘性爬行为中等深度地震提供了可行的机制.
  • 这种机制解释了发生在比脱水可能更深处的地震.
  • 该模型预测这些地震事件的周期性.