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Videos de Conceptos Relacionados

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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Video Experimental Relacionado

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

Difusión protónica en hielo de alta presión VII

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
Resumen

La difusión protónica en hielo VII se midió a altas presiones. Los resultados muestran que la difusión protónica sigue siendo lenta, no alcanzando los criterios superiónicos ni siquiera cerca del punto de fusión.

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Área de la Ciencia:

  • La geofísica es la geofísica.
  • Ciencia de los materiales Ciencia de los materiales.
  • Química Física es la química física.

Sus antecedentes:

  • La difusión molecular típicamente domina la difusión protónica en hielo a presiones ambientales.
  • Los modelos teóricos sugieren que la difusión protónica puede llegar a ser dominante en el hielo bajo condiciones de alta presión.

Objetivo del estudio:

  • Para determinar experimentalmente el coeficiente de difusión protónica en hielo VII a través de su rango de presión estable.
  • Para investigar el comportamiento dependiente de la presión de la difusión protónica en la fase molecular de más alta temperatura del hielo.

Principales métodos:

  • Las mediciones del coeficiente de difusión protónica se llevaron a cabo en hielo VII a 400 kelvin.
  • Los experimentos cubrieron toda la región de presión estable para el hielo VII, de 10 a 63 gigapascals.

Principales resultados:

  • Los coeficientes de difusión protónica medidos oscilaron entre 10−17 y 10−15 m2/s.
  • Los coeficientes de difusión extrapolados cerca de la curva de fusión del hielo VII fueron de 100 a 1000 veces más bajos que el criterio superiónico.

Conclusiones:

  • La difusión protónica en hielo VII no se acerca al régimen superiónico bajo las condiciones estudiadas de alta presión y alta temperatura.
  • Los hallazgos experimentales contrastan con las predicciones teóricas de difusión protónica dominante a altas presiones.