text: Carbon sequestration is the process of storing carbon in a carbon pool. It plays a crucial role in mitigating climate change by reducing the amount of carbon dioxide in the atmosphere. There are two main types of carbon sequestration: biologic (also called biosequestration) and geologic. Biologic carbon sequestration is a naturally occurring process as part of the carbon cycle. Humans can enhance it through deliberate actions and use of technology. Carbon dioxide () is naturally captured from the atmosphere through biological, chemical, and physical processes. These processes can be accelerated for example through changes in land use and agricultural practices, called carbon farming. Artificial processes have also been devised to produce similar effects. This approach is called carbon capture and storage. It involves using technology to capture and sequester (store)  that is produced from human activities underground or under the sea bed.  
  Forests, kelp beds, and other forms of plant life absorb carbon dioxide from the air as they grow, and bind it into biomass. However, these biological stores are considered impermanent carbon sinks as the long-term sequestration cannot be guaranteed. For example, natural events, such as wildfires or disease, economic pressures and changing political priorities can result in the sequestered carbon being released back into the atmosphere.
  Carbon dioxide that has been removed from the atmosphere can also be stored in the Earths crust by injecting it into the subsurface, or in the form of insoluble carbonate salts. The latter process is called mineral sequestration. These methods are considered non-volatile' because they not only remove carbon dioxide from the atmosphere but also sequester it indefinitely. This means the carbon is "locked away" for thousands to millions of years.
  To enhance carbon sequestration processes in oceans the following technologies have been proposed: Seaweed farming, ocean fertilization, artificial upwelling, basalt storage, mineralization and deep sea sediments, adding bases to neutralize acids. However, none have achieved large scale application so far.