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Published on: February 25, 2015
Multiphase Flow Regime Controls Carbonate Precipitation Morphologies during CO2 Injection in Subsurface Basalts
Tianxiao Shen1, Quin R S Miller2, Nabajit Lahiri2
1Department of Earth and Environmental Engineering, Columbia University, New York, NY 10027, United States.
Simulations of CO2-water flow in basalt cores reveal how flow dynamics and pore structure control carbonate nodule formation. This research links computational fluid dynamics models to real-world crystallization in subsurface reservoirs.
Area of Science:
- Geochemistry and Subsurface Science
- Computational Fluid Dynamics (CFD)
- Petroleum Engineering and Carbon Sequestration
Background:
- The Wallula Basalt Pilot Demonstration (WBPD) is the first supercritical CO2 injection test in a basalt reservoir.
- Understanding multiphase flow dynamics in basalt is crucial for predicting CO2 storage security and mineral precipitation.
- Previous studies lacked detailed pore-scale insights into CO2-water interactions and subsequent carbonate formation in basalt.
Purpose of the Study:
- To investigate basalt multiphase flow dynamics using pore-scale simulations and experimental data.
- To determine the influence of flow parameters (capillary number, water saturation) on carbonate nodule formation.
- To link computational fluid dynamics (CFD) models with observed postinjection crystallization behaviors in a basalt testbed.
Main Methods:
- Pore-scale Lattice Boltzmann Method (LBM) CFD simulations on core samples from the WBPD.
- Integration of micro-CT, optical microscopy, SEM, N2 adsorption, and low-field NMR for pore structure and fluid analysis.
- Application of transition state theory to model carbonate precipitation mechanisms.
Main Results:
- Simulations revealed distinct CO2-water interface distributions in connected (Zone 1) versus semi-isolated (Zone 2) vesicles.
- Flow regimes in Zone 1 limit the size of small carbonate precipitates (<35 μm).
- In Zone 2, large carbonate nodules (0.2-2 mm) formation is controlled by the interplay of CO2-water interfaces and vesicle surface alterations, creating favorable conditions for growth.
Conclusions:
- Morphology-determined local water saturation and pH gradients drive supersaturation, favoring carbonate growth in basalt vesicles.
- The study proposes stepwise mechanisms for carbonate precipitation, enhancing geochemical and reactive transport models for basaltic lithologies.
- This work establishes a direct link between a posteriori CFD modeling and observed postinjection crystallization in a real-world subsurface environment.
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