Deep Saline Aquifers - CCUS Terms
Description:
Deep Saline Aquifers are underground layers of porous rock saturated with saline water, typically located at depths greater than 800 meters. These formations can store large amounts of carbon dioxide (CO₂) injected into them.
Explanation:
In the context of Carbon Capture, Utilization, and Storage (CCUS), deep saline aquifers are considered a significant option for the long-term storage of captured CO₂. Here’s how deep saline aquifers work and their importance within the broader CCUS framework:
Advantages:
Storing CO₂ in deep saline aquifers helps reduce GHG emissions by preventing CO₂ from reaching the atmosphere, supporting international climate goals and commitments like the Paris Agreement; it provides a cost-effective method for storing large volumes of CO₂, reducing costs and promoting profitability for businesses and industries involved in CO₂ storage, while clear and transparent storage processes help build public trust and acceptance of CCUS projects, ensuring community support and participation.
Challenges:
Implementing CO₂ storage in deep saline aquifers can be technically complex and require significant expertise, making sound science and engineering principles crucial for success; securing sufficient funding and resources for CO₂ storage projects can be challenging, necessitating adequate investment for the success of storage initiatives; and navigating regulatory requirements and market barriers can be difficult, requiring clear and supportive policies to foster the development and deployment of CO₂ storage technologies.
In summary, Deep Saline Aquifers are essential for promoting the development and deployment of Carbon Capture, Utilization, and Storage technologies. By providing a secure environment for the long-term storage of CO₂, they help reduce greenhouse gas emissions and contribute to global efforts to mitigate climate change.