PapersFlow Research Brief

Physical Sciences · Environmental Science

CO2 Sequestration and Geologic Interactions
Research Guide

What is CO2 Sequestration and Geologic Interactions?

CO2 sequestration and geologic interactions refer to the geological storage of carbon dioxide in deep sedimentary formations such as saline aquifers, involving geochemical processes like mineral carbonation, reactive transport modeling, and caprock integrity to mitigate climate change.

This field encompasses 59,431 papers on geological storage of CO2, covering mineral carbonation, reactive transport modeling, caprock integrity, and saline aquifers for long-term storage. Parkhurst and Appelo (1999) introduced PHREEQC version 2, a program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations, with 7668 citations. The IPCC special report by Metz et al. (2021) assesses technical, scientific, environmental, economic, and societal aspects of CO2 capture and storage, cited 4922 times.

Topic Hierarchy

100%
graph TD D["Physical Sciences"] F["Environmental Science"] S["Environmental Engineering"] T["CO2 Sequestration and Geologic Interactions"] D --> F F --> S S --> T style T fill:#DC5238,stroke:#c4452e,stroke-width:2px
Scroll to zoom • Drag to pan
59.4K
Papers
N/A
5yr Growth
635.2K
Total Citations

Research Sub-Topics

Why It Matters

CO2 sequestration in geologic formations enables mitigation of climate change by storing emissions from fossil fuel power stations in saline aquifers and deep sedimentary basins. Bui et al. (2018) in 'Carbon capture and storage (CCS): the way forward' outline CCS applications across industries, including emissions offsets and net negative emissions from atmospheric CO2 removal. Leung et al. (2014) in 'An overview of current status of carbon dioxide capture and storage technologies' detail CCS strategies to meet global CO2 reduction targets, with power generation and cement production as key sectors. Boot-Handford et al. (2013) in 'Carbon capture and storage update' note that gas, coal, and biomass-fired stations using CCS prevent atmospheric CO2 emissions while responding to energy demand changes.

Reading Guide

Where to Start

"User's guide to PHREEQC (Version 2): A computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations" by Parkhurst and Appelo (1999), as it provides foundational tools for modeling geochemical interactions essential to all CO2 sequestration studies.

Key Papers Explained

Parkhurst and Appelo (1999) establish PHREEQC for geochemical calculations, extended in their 2013 version 3 with advanced aqueous models. Metz et al. (2021) IPCC report contextualizes these tools within CCS assessment, while Bui et al. (2018) apply them to practical deployment across sectors. Leung et al. (2014) overview connects modeling to technology status, and Boot-Handford et al. (2013) update links to power station applications.

Paper Timeline

100%
graph LR P0["Carbon dioxide in water and seaw...
1974 · 3.4K cites"] P1["User's guide to PHREEQC Version...
1999 · 7.7K cites"] P2["A marine microbial consortium ap...
2000 · 3.1K cites"] P3["Stabilization Wedges: Solving th...
2004 · 3.1K cites"] P4["Description of input and example...
2013 · 3.5K cites"] P5["Carbon capture and storage CCS ...
2018 · 3.9K cites"] P6["IPCC special report on carbon di...
2021 · 4.9K cites"] P0 --> P1 P1 --> P2 P2 --> P3 P3 --> P4 P4 --> P5 P5 --> P6 style P1 fill:#DC5238,stroke:#c4452e,stroke-width:2px
Scroll to zoom • Drag to pan

Most-cited paper highlighted in red. Papers ordered chronologically.

Advanced Directions

Current work builds on PHREEQC for reactive transport in caprock integrity, with focus on saline aquifers and mineral carbonation kinetics from established models. No recent preprints available, so frontiers emphasize integrating PHREEQC version 3 outputs with field data from IPCC-assessed sites.

Papers at a Glance

Frequently Asked Questions

What is PHREEQC used for in CO2 sequestration modeling?

PHREEQC version 2, developed by Parkhurst and Appelo (1999), performs low-temperature aqueous geochemical calculations including speciation, saturation-index, batch-reaction, one-dimensional transport, and inverse calculations based on ion-association models. PHREEQC version 3 by the same authors (2013) extends these capabilities with C and C++ implementation and additional aqueous models like the Lawrence Livermore National Laboratory model. These tools model reactive transport and geochemical interactions in geologic CO2 storage.

How does the IPCC assess CO2 capture and storage?

The IPCC special report on carbon dioxide capture and storage by Metz et al. (2021) evaluates technical, scientific, environmental, economic, and societal dimensions of CCS for climate mitigation. It examines CO2 storage potential in geologic formations like saline aquifers. The report serves as a comprehensive assessment of CCS deployment feasibility.

What are key geologic formations for CO2 storage?

Saline aquifers and deep sedimentary formations provide capacity for long-term CO2 storage through physical trapping and geochemical interactions. Caprock integrity ensures containment by preventing leakage. Mineral carbonation converts CO2 into stable carbonates via reactions with reservoir minerals.

What processes model CO2 interactions in geology?

Reactive transport modeling simulates CO2 migration, dissolution, and mineral reactions in aquifers. Geochemical modeling with tools like PHREEQC computes speciation and saturation indices during injection. These methods predict caprock sealing and long-term storage security.

Why is caprock integrity critical in CO2 sequestration?

Caprock acts as a seal to trap supercritical CO2 in reservoirs beneath low-permeability layers. Integrity assessments evaluate geochemical alteration and mechanical stability post-injection. Modeling ensures containment over millennia-scale storage periods.

Open Research Questions

  • ? How do long-term geochemical reactions affect caprock permeability in saline aquifer storage?
  • ? What reactive transport parameters best predict mineral carbonation rates in deep sedimentary formations?
  • ? Which factors control CO2 leakage risks through faulted caprocks?
  • ? How do microbial processes influence anaerobic CO2 oxidation in marine geologic reservoirs?
  • ? What scaling factors bridge lab-scale weathering rates to field-scale sequestration efficiency?

Research CO2 Sequestration and Geologic Interactions with AI

PapersFlow provides specialized AI tools for Environmental Science researchers. Here are the most relevant for this topic:

See how researchers in Earth & Environmental Sciences use PapersFlow

Field-specific workflows, example queries, and use cases.

Earth & Environmental Sciences Guide

Start Researching CO2 Sequestration and Geologic Interactions with AI

Search 474M+ papers, run AI-powered literature reviews, and write with integrated citations — all in one workspace.

See how PapersFlow works for Environmental Science researchers