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Related Concept Videos

Phase Diagrams02:39

Phase Diagrams

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A phase diagram combines plots of pressure versus temperature for the liquid-gas, solid-liquid, and solid-gas phase-transition equilibria of a substance. These diagrams indicate the physical states that exist under specific conditions of pressure and temperature and also provide the pressure dependence of the phase-transition temperatures (melting points, sublimation points, boiling points). Regions or areas labeled solid, liquid, and gas represent single phases, while lines or curves represent...
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Carbonation is a process used to dissolve carbon dioxide gas in a liquid, commonly used in the production of carbonated beverages. Achieving efficient carbonation requires careful control of temperature, pressure, and flow conditions. By adjusting these parameters, carbonation efficiency can be maximized, producing a higher concentration of CO2 in the liquid.
Temperature is a key factor in CO2 solubility. In this case, the CO2 gas and the liquid are cooled to 20°C. Lower temperatures...
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Updated: Jun 21, 2025

Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography
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A Pore-Scale Phase Field Model for CO2-Fluid-Basalt Interactions.

Wenchao Dou1, Changxi Geng2, Mian Lin1,3

  • 1Key Laboratory for Mechanics in Fluid Solid Coupling Systems, Institute of Mechanics, Chinese Academy of Sciences, Beijing 100190, China.

ACS Omega
|July 8, 2024
PubMed
Summary

Basalt

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Area of Science:

  • Geochemistry
  • Geology
  • Materials Science

Background:

  • Basalt formations are promising for geological carbon dioxide (CO2) storage.
  • Understanding CO2-fluid-basalt interactions is vital for safe CO2 sequestration.
  • Pore structure evolution impacts storage capacity and integrity.

Purpose of the Study:

  • To model CO2-fluid-basalt interactions at the pore scale.
  • To investigate the impact of these interactions on basalt's pore structure.
  • To assess the influence of temperature and pressure on reaction rates for site selection.

Main Methods:

  • A pore-scale phase field model was developed.
  • The model simulates CO2-fluid-basalt reactions using real 3D rock images.
  • Simulations analyzed mineral dissolution, precipitation, and porosity changes over 120 days.

Main Results:

  • Secondary mineral precipitation (3.75%) exceeded mineral dissolution (2.01%).
  • Porosity decreased by 1.74%, significantly reducing pore connectivity.
  • Higher temperatures and pressures accelerated reaction rates, with temperature having a greater effect.

Conclusions:

  • CO2 sequestration in basalt leads to reduced porosity and altered pore structure.
  • High geothermal gradients are favorable for accelerating CO2-basalt reactions.
  • The model provides insights for optimizing CO2 geological storage site selection.