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Porosity and Absorption of Aggregate01:20

Porosity and Absorption of Aggregate

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Aggregates contain pores of varying sizes; while some are completely enclosed within the particles, others open onto the surface, allowing water to penetrate. The porosity of aggregates is a major factor contributing to the overall porosity of concrete, given that aggregates constitute about three-quarters of concrete's volume.
When all pores in an aggregate are filled with water, the aggregate is considered saturated and surface-dry. If left in dry air, water will evaporate until the...
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Phase Transitions: Vaporization and Condensation02:39

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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...
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Permeability of Concrete01:25

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Permeability in the context of concrete refers to how easily liquids or gases can pass through the material. This quality is crucial for assessing the water-tightness and durability of concrete structures and their resistance to chemical attacks. Concrete permeability can be determined through comparative laboratory tests. These tests typically involve sealing a concrete specimen from the sides, applying water pressure to the top surface with pressure, and measuring the amount of water passing...
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Phase Transitions: Sublimation and Deposition02:33

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Types of Coprecipitation01:10

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Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
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Colloidal precipitates01:09

Colloidal precipitates

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The high insolubility of some precipitates can result in an unfavorable relative supersaturation. This can lead to colloidal particles with a large surface-to-mass ratio, where adsorption is promoted. For instance, in the precipitation of silver chloride, silver ions are adsorbed on the surface of the colloidal particles, forming a primary layer. This layer attracts ions of opposite charge (such as nitrate ions), forming a diffuse secondary layer of adsorbed ions. This electric double layer...
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Surface properties of alkali silicate glasses: Influence of the modifiers.

The Journal of chemical physics·2023
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Updated: Oct 14, 2025

Fluid-cell Raman Spectroscopy for operando Studies of Reaction and Transport Phenomena during Silicate Glass Corrosion
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Fluid-cell Raman Spectroscopy for operando Studies of Reaction and Transport Phenomena during Silicate Glass Corrosion

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Transiciones de percolación en vidrios comprimidos de SiO2

A Hasmy1,2, S Ispas3, B Hehlen4

  • 1Laboratoire Charles Coulomb (L2C), CNRS - Université Montpellier, Montpellier, France. anwarhasmy@hotmail.com.

Nature
|November 4, 2021
PubMed
Resumen

Los cambios estructurales en el vidrio de sílice comprimido bajo presión se producen a través de transiciones de percolación. Estas transiciones explican anomalías mecánicas e irreversibilidad, revelando nuevos estados amorfos y vías.

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Área de la Ciencia:

  • Ciencias de los materiales
  • Física de la materia condensada
  • Química computacional

Sus antecedentes:

  • Las transformaciones amorfas bajo presión se explican típicamente por cambios estructurales locales.
  • El papel de la invarianza de escala y los umbrales críticos en estas transformaciones sigue sin estar claro.
  • Comprender estas transiciones es crucial para la ciencia de los materiales y la física de la materia condensada.

Objetivo del estudio:

  • Investigar el mecanismo de las transformaciones amorfas en vidrio de sílice comprimido.
  • Para determinar si estas transformaciones exhiben características similares a las transiciones de fase verdaderas.
  • Explorar la aplicabilidad de la teoría de la percolación a los cambios estructurales inducidos por la presión en materiales amorfos.

Principales métodos:

  • Se utilizaron cálculos basados en ab initio para simular el vidrio de sílice comprimido (SiO2).
  • El estudio analizó los cambios estructurales de estados amorfos de baja a alta densidad.
  • La teoría de la percolación se usó para modelar la aparición de grupos estructurales interconectados.

Principales resultados:

  • Los cambios estructurales ocurren a través de una secuencia de transiciones de percolación, no solo reorganizaciones locales.
  • Aparición de grupos de poliedros de largo alcance (tetraedros, pentaedros, octaedros) a presiones críticas.
  • El mecanismo explica las anomalías mecánicas (por ejemplo, a 3 GPa) y la irreversibilidad estructural (más allá de 10 GPa).
  • Las estructuras amorfas descubiertas se asemejan a los cristales de coesita IV y V, enfatizando el papel del pentaedro SiO5.

Conclusiones:

  • La teoría de la percolación proporciona un marco robusto para comprender las transformaciones amorfas bajo presión.
  • Los hallazgos ofrecen información sobre el proceso de densificación de la sílice vítrea.
  • Este trabajo abre nuevas vías para predecir fases sólidas y líquidas amorfas desconocidas.