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相关概念视频

Isothermal Processes01:21

Isothermal Processes

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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...
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Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

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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...
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Frictional Forces on Flat Belts01:28

Frictional Forces on Flat Belts

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Flat belts are commonly used in various industrial applications for transmitting power from one pulley to another. When a flat belt is wrapped around a set of pulleys, it experiences different tensions at the driving pulley ends due to the friction between the belt and pulley surface. When the pulley moves in a counterclockwise direction, the tension T2 on the opposite side of the pulley where the belt is moving away from is higher than the tension T1 on the side where the belt is moving...
904
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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Frictional Forces on Screws01:17

Frictional Forces on Screws

1.2K
Screws are characterized by a helical ridge known as a thread wrapped around a cylindrical shaft. They are commonly used as fasteners to hold objects together or to transmit power and motion in machines. One type of screw that is particularly useful for transmitting power is the square-threaded screw.
A jack with a square-threaded screw is a mechanical device used to lift heavy loads by applying a force at its handle. When the force is applied, the screw turns, raising the load. The screw can...
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Elastic Strain Energy for Shearing Stresses01:20

Elastic Strain Energy for Shearing Stresses

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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...
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Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
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超级压力锁定编码在俯冲景观中的超级压力锁定.

Bar Oryan1,2, Jean-Arthur Olive1, Romain Jolivet1,3

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Science advances
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概括

俯冲巨型推力锁定产生了压力,在数千年内塑造了景观. 这项研究揭示了这种被视为地震和升起的地震间应变如何影响潜伏区的地形学.

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科学领域:

  • 地质物理学 地质物理学
  • 构造学 构造学 构造学 构造学
  • 地质形态学 地质形态学

背景情况:

  • 俯冲巨型冲击显示了封闭区域和景观特征之间的相关性.
  • 连接大压力锁定与地形学之间的机制尚不清楚.

研究的目的:

  • 调查从俯冲巨推力锁定中产生的间地震应变如何影响超越板块变形和景观演变.
  • 为了解释在俯冲区中观察到的地形特征.

主要方法:

  • 建模跨地震应变积累和释放在覆盖板块上的模式.
  • 分析应变增加和长期抬起模式之间的关系.
  • 将建模的升起与观察到的地形特征连接起来,例如河流概况和海洋露台.

主要成果:

  • 地震间锁定梯度产生分布式地震性和不可逆转的应变.
  • 总结地震周期的应变增量,就产生了空间变量的升起.
  • 这种长期的升起解释了潜水区的关键地质形态特征,包括架子断层,海洋露台和河流形状.

结论:

  • 不弹性前弓的产量编码大推力锁定模式到景观中.
  • 在多次地震周期中,巨型冲击锁定似乎稳定.
  • 地形学可以作为一个有价值的工具来限制潜水带的地震危险.