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関連する概念動画

Phase Transitions: Vaporization and Condensation02:39

Phase Transitions: Vaporization and Condensation

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...
Vapor Pressure02:34

Vapor Pressure

When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase molecules move randomly about, they will occasionally collide with the surface of the condensed phase, and in some cases, these collisions will result in the molecules re-entering the condensed phase. The change from the gas phase to the liquid is called condensation. When the rate of condensation becomes equal to the rate of vaporization, neither the amount of the liquid nor the amount of the vapor...
Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

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...
Vapor Pressure Lowering03:28

Vapor Pressure Lowering

The equilibrium vapor pressure of a liquid is the pressure exerted by its gaseous phase when vaporization and condensation are occurring at equal rates: Dissolving a nonvolatile substance in volatile liquid results in a lowering of the liquid’s vapor pressure. This phenomenon can be explained by considering the effect of added solute molecules on the liquid's vaporization and condensation processes. To vaporize, solvent molecules must be present at the surface of the solution. The presence of...
Excess Pressure Inside a Drop and a Bubble01:13

Excess Pressure Inside a Drop and a Bubble

The shape of a small drop of liquid can be considered spherical, neglecting the effect of gravity. This drop can further be considered as two equal hemispherical drops put together due to surface tension. The forces acting on the spherical drop are due to the pressure of the liquid inside the drop, the pressure due to air outside the drop, and the force due to the surface tension acting on the two hemispherical drops.
Vapor Pressure of Fluid01:28

Vapor Pressure of Fluid

The vapor pressure of a fluid is a crucial concept in fluid mechanics, influencing phenomena such as boiling and cavitation. Vapor pressure refers to the pressure exerted by a vapor at a state of thermodynamic equilibrium with its corresponding liquid phase at a specific temperature. It represents the tendency of molecules to escape from the fluid surface into the vapor phase.
When a liquid is placed in a closed container with a small air space, and the space is evacuated, vapor molecules will...

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関連する実験動画

Updated: Jul 11, 2026

High Pressure Single Crystal Diffraction at PX^2
11:32

High Pressure Single Crystal Diffraction at PX^2

Published on: January 16, 2017

高圧氷 VII でのプロトン拡散

Eriko Katoh1, H Yamawaki, H Fujihisa

  • 1National Institute of Advanced Industrial Science and Technology, Tsukuba Central 5, Tsukuba 305-8565, Ibaraki, Japan.

Science (New York, N.Y.)
|February 16, 2002
PubMed
まとめ

氷 VII のプロトン拡散は,高圧で測定されました. 結果は,陽子拡散が遅いまま,融点に近いところでも超陽子基準に達しないことを示しています.

科学分野:

  • 地質物理学 地質物理学とは地質物理学です.
  • 材料科学 材料科学とは
  • 物理化学 物理化学

背景:

  • 分子拡散は,通常,周囲の圧力下での氷の陽子拡散を支配する.
  • 理論的なモデルは,高圧条件下でプロトン拡散が氷の中で支配的になる可能性があることを示唆しています.

研究 の 目的:

  • 氷 VII の安定した圧力範囲全体で陽子拡散係数を実験的に決定する.
  • 氷の最も高温の分子相における陽子拡散の圧力依存的振る舞いを調査する.

主な方法:

  • 陽子拡散係数の測定は,ケルビン400度の氷VII上で行われました.
  • 実験は10から63ギガパスカルの氷VIIの安定圧力領域全体をカバーしました.

主要な成果:

  • 測定されたプロトン拡散係数は10−17から10−15 m2/sの範囲であった.
  • 氷の溶解曲線VIIの近くの外積分された拡散係数は,スーパーイオン基準より100~1000倍低かった.

結論:

  • 氷VIIにおけるプロトン拡散は,研究された高圧および高温条件下では,スーパーイオン状態に近づかない.
  • 実験的発見は,高圧で支配的な陽子拡散の理論的予測と対照的である.

さらに関連する動画

Achieving Moderate Pressures in Sealed Vessels Using Dry Ice As a Solid CO2 Source
06:26

Achieving Moderate Pressures in Sealed Vessels Using Dry Ice As a Solid CO2 Source

Published on: August 17, 2018

An Externally-Heated Diamond Anvil Cell for Synthesis and Single-Crystal Elasticity Determination of Ice-VII at High Pressure-Temperature Conditions
07:48

An Externally-Heated Diamond Anvil Cell for Synthesis and Single-Crystal Elasticity Determination of Ice-VII at High Pressure-Temperature Conditions

Published on: June 18, 2020

関連する実験動画

Last Updated: Jul 11, 2026

High Pressure Single Crystal Diffraction at PX^2
11:32

High Pressure Single Crystal Diffraction at PX^2

Published on: January 16, 2017

Achieving Moderate Pressures in Sealed Vessels Using Dry Ice As a Solid CO2 Source
06:26

Achieving Moderate Pressures in Sealed Vessels Using Dry Ice As a Solid CO2 Source

Published on: August 17, 2018

An Externally-Heated Diamond Anvil Cell for Synthesis and Single-Crystal Elasticity Determination of Ice-VII at High Pressure-Temperature Conditions
07:48

An Externally-Heated Diamond Anvil Cell for Synthesis and Single-Crystal Elasticity Determination of Ice-VII at High Pressure-Temperature Conditions

Published on: June 18, 2020