Multiphase Flow Regime Controls Carbonate Precipitation Morphologies during CO<sub>2</sub> Injection in Subsurface Basalts

Pore-scale CO<sub>2</sub>-H<sub>2</sub>O multiphase flow simulations were performed on domains extracted from first-of-their-kind postinjection sidewall cores retrieved from Pacific Northwest National Lab's Wallula Basalt Pilot Demonstration (WBPD), the world's first supercritical CO<sub>2</sub> injection test in a basalt reservoir. We integrate Lattice Boltzmann Method computational fluid dynamics (CFD) simulations , pore-scale imaging (micro-CT, optical microscopy, SEM), and transition state theory to investigate basalt multiphase flow dynamics and the influence of multiphase flow parameters (capillary number, Ca#, and water saturation) on the occurrence of small (<35 μm) and large (0.2-2 mm) postinjection carbonate nodules within, respectively, WBPD Zone 1 (connected vesicles) and Zone 2 (semi-isolated vesicles) end-members. Image analysis is augmented by pore size distribution measurements (N<sub>2</sub> adsorption, low-field NMR) to establish the dual-porosity nature of the zones and subvoxel resolution fluid flow pathways to vesicles. In Zone 1, drainage simulations demonstrate how the distribution of scCO<sub>2</sub>-water interfaces vary under different capillary and viscous flow regimes and may limit the size of precipitants. In Zone 2, 3D morphological analysis of simulated capillary-driven scCO<sub>2</sub>-water distributions and microCT-informed carbonate growth within vesicles reveals that the location and growth extent of large carbonate nodules are likely controlled by the distribution of scCO<sub>2</sub>-water interfaces (acidity source) in relation to altered vesicle surfaces (alkalinity source). Toward augmenting geochemical/reactive transport models in basalt lithologies and beyond, we propose stepwise mechanisms describing how morphology-determined local water saturation and pH gradients lead to supersaturated "Goldilocks region" conditions favorable for carbonate growth. This work directly links <i>a posteriori</i> CFD models to postinjection crystallization behaviors in a subsurface testbed.

Authors

Institutions

Publication Details

Journal
Environmental Science & Technology
Published
2025-09-16
DOI
https://doi.org/10.1021/acs.est.5c03397
Citations
6
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
4.79
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Multiphase Flow Regime Controls Carbonate Precipitation Morphologies during CO2 Injection in Subsurface Basalts

Olivia Terry, Zuhao Kou, Herbert T. Schaef, Quin R. S. Miller et al.
6 citations
Environmental Science & Technology
CO2 Sequestration and Geologic Interactions
4.79
article

Multiphase Flow Regime Controls Carbonate Precipitation Morphologies during CO2 Injection in Subsurface Basalts

Olivia Terry, Zuhao Kou, Herbert T. Schaef, Quin R. S. Miller, Shaina Kelly, Nabajit Lahiri, Antoinette T. Owen, Ting Shen
article en
6 citations

Abstract

Pore-scale CO<sub>2</sub>-H<sub>2</sub>O multiphase flow simulations were performed on domains extracted from first-of-their-kind postinjection sidewall cores retrieved from Pacific Northwest National Lab's Wallula Basalt Pilot Demonstration (WBPD), the world's first supercritical CO<sub>2</sub> injection test in a basalt reservoir. We integrate Lattice Boltzmann Method computational fluid dynamics (CFD) simulations , pore-scale imaging (micro-CT, optical microscopy, SEM), and transition state theory to investigate basalt multiphase flow dynamics and the influence of multiphase flow parameters (capillary number, Ca#, and water saturation) on the occurrence of small (<35 μm) and large (0.2-2 mm) postinjection carbonate nodules within, respectively, WBPD Zone 1 (connected vesicles) and Zone 2 (semi-isolated vesicles) end-members. Image analysis is augmented by pore size distribution measurements (N<sub>2</sub> adsorption, low-field NMR) to establish the dual-porosity nature of the zones and subvoxel resolution fluid flow pathways to vesicles. In Zone 1, drainage simulations demonstrate how the distribution of scCO<sub>2</sub>-water interfaces vary under different capillary and viscous flow regimes and may limit the size of precipitants. In Zone 2, 3D morphological analysis of simulated capillary-driven scCO<sub>2</sub>-water distributions and microCT-informed carbonate growth within vesicles reveals that the location and growth extent of large carbonate nodules are likely controlled by the distribution of scCO<sub>2</sub>-water interfaces (acidity source) in relation to altered vesicle surfaces (alkalinity source). Toward augmenting geochemical/reactive transport models in basalt lithologies and beyond, we propose stepwise mechanisms describing how morphology-determined local water saturation and pH gradients lead to supersaturated "Goldilocks region" conditions favorable for carbonate growth. This work directly links <i>a posteriori</i> CFD models to postinjection crystallization behaviors in a subsurface testbed.

Environmental Science & TechnologyVol. 59(38)
Pacific Northwest National Laboratory (US), Columbia University (US)
Openalex Percentile: Top 5%
CO2 Sequestration and Geologic Interactions
4.79
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.