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相关概念视频

Vaporization01:18

Vaporization

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The physical form of a substance changes by changing its temperature. For example, raising the temperature of a liquid causes the liquid to vaporize (convert into vapor). The process is called vaporization—a surface phenomenon. For vaporization to occur, kinetic energy must be greater than the intermolecular forces that keep molecules bonded. The amount of energy needed to vaporize a quantity of liquid at a given pressure and a constant temperature is called the heat of vaporization. When...
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Veins01:17

Veins

9.5K
Veins are an integral part of our circulatory system, serving as the blood vessels that transport blood from all body regions to the heart. They are a network of hollow tubes that carry blood low in oxygen from the body's cells back to the heart for reoxygenation. Veins are crucial for maintaining the body's overall fluid balance and the continuous circulation of blood.
Structure of Veins:
The structure of veins is specifically designed to assist in the low-pressure transportation of...
9.5K
Phase Transitions: Vaporization and Condensation02:39

Phase Transitions: Vaporization and Condensation

22.1K
The physical form of a substance changes on changing its temperature. For example, raising the temperature of a liquid causes the liquid to vaporize (convert into vapor). The process is called vaporization—a surface phenomenon. Vaporization occurs when the thermal motion of the molecules overcome the intermolecular forces, and the molecules (at the surface) escape into the gaseous state. When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase molecules...
22.1K
Volatilization01:10

Volatilization

6.4K
Volatilization gravimetry is an analytical technique that measures the mass lost due to the volatilization of the substance. This technique is used to estimate the amount of volatile material in a sample. To perform this method, heat a known amount of the sample to a high temperature in a crucible or other suitable vessel. The volatile substance in the sample evaporates, and the vapor is completely expelled from the crucible either by heating the sample or bubbling a stream of inert gas through...
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Pinching-off of Coated Vesicles01:32

Pinching-off of Coated Vesicles

4.4K
Vesicle budding is orchestrated by distinct cytosolic proteins such as adaptor proteins, coat proteins, and GTPases. To initiate vesicle budding, membrane-bending proteins containing crescent-shaped BAR domains bind to the lipid heads in the bilayer and distort the membrane to form a protein-coated vesicle bud. Adaptors proteins such as AP2 for clathrin-coated vesicles can nucleate on the deformed membrane. Finally, coat proteins such as clathrin or COPI and COPII assemble into a coat forming...
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Vascular Spasm01:16

Vascular Spasm

4.8K
The vascular phase, also known as vasospasm, is the initial stage of hemostasis, crucial for preventing excessive bleeding when a blood vessel is injured. After a vessel is cut, nerves in the damaged area trigger pain and other sensory impulses. Simultaneously, the smooth muscles in the vessel wall contract, resulting in a vascular spasm. This contraction reduces the vessel's diameter at the injury site, slowing or stopping blood loss through the vessel wall. Vascular spasms typically last...
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相关实验视频

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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
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火山爆发期间的热囊

Yan Lavallée1, Donald B Dingwell2, Jeffrey B Johnson3

  • 1Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool L69 3GP, UK.

Nature
|December 25, 2015
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概括
此摘要是机器生成的。

不仅仅是压力下降,而热也会导致火山爆发, 这项研究揭示了摩擦加热如何溶解岩,影响喷发风格和爆炸性.

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科学领域:

  • 火山学
  • 地质化学
  • 石油学

背景情况:

  • 火山爆发是由岩升起所驱动的,而水泡形成会降低岩的密度和强度.
  • 传统上,岩脱气和囊泡与压缩和依赖压力的水溶性有关.
  • 温度依赖的水溶性和岩加热在囊泡中的作用在很大程度上被忽视了.

研究的目的:

  • 研究岩加热对囊泡和碎片化的影响,并将其与压缩驱动的过程对比.
  • 探索摩擦加热在产生热量的潜力,用于融和囊泡.
  • 重新评估控制岩脱气,强度和喷发风格的因素.

主要方法:

  • 来自危地马拉圣地亚吉托火山的火山灰纹理的现场分析.
  • 实验室对断层摩擦进行实验,以模拟岩的升温和融化.
  • 在不同温度和压力条件下测定岩中的水溶性.

主要成果:

  • 结构分析显示火山灰中含有微泡的化学异质纤维,
  • 摩擦加热实验表明,摩擦可以产生足够的热量来诱导水化性岩的融化和化.
  • 实验数据表明,加热可以成为许多岩上升路径的水溶解的更有效的驱动因素.

结论:

  • 通过晶体的潜热或摩擦加热等机制,热显著影响脱气和囊泡.
  • 在上升过程中,岩的热历史对岩强度和涌和爆炸性喷发之间的过渡是一个关键的控制.
  • 这项研究强调了在了解火山爆发动态时考虑热过程与解压的重要性.