Carbon storage refers to the process of safely and permanently storing the CO2 captured from power plants and industrial processes.
Before CO2 can be transported it must first be compressed at high pressure into a liquid-like state. The technologies available to transport CO2 are very similar to those used for many years in the natural gas industry. However, unlike natural gas, CO2 is essentially a stable and inert substance.
The best way to transport CO2 depends on the quantity, terrain and transport distance required. Tanker trucks may be used for smaller volumes over short distances. Pipelines are a logical choice for large volumes over short, medium or long overland distances. Thousands of kilometres of CO2 pipeline are already in existence in the US, and have been safely transporting CO2 for Enhanced Oil Recovery for many years.
The next step is storage. While there are a number of CO2 storage options, geological storage or geosequestration offers the greatest potential. This involves safely storing captured, liquefied, and transported CO2 deep underground. A common misconception is that these storage sites are like vast caves or caverns underground. In fact, they consist of tiny pores within the rock, which act like a sponge to house the liquefied CO2. These tiny pores add up to a huge volume, with the capacity to store millions of tonnes of CO2. They are overlain by a non-porous ‘cap’ rock that prevents the CO2 from escaping.
There are three main categories of geological storage options for CO2. The first is saline water saturated rocks. These are underground formations of porous rock, such as sandstones, that are saturated with salty (non potable) water and covered by a layer of impermeable cap rock (such as shale or clay), which acts as a seal. Once injected into the formation, the CO2 dissolves into the saline water in the reservoir rock. CO2 storage in deep saline formations is expected to take place at depths below 800m. At this depth, the CO2 will be at high enough pressures to remain in a liquid-like state. Saline formations have the largest storage potential globally and a number of CO2 storage demonstration projects are proving their effectiveness to maximise storage capacity and containment.
The second main type of geological storage is depleted oil and gas fields. These have a proven ability to store hydrocarbons over millions of years, demonstrating very good reservoir characteristics.[PDF] CO2 injection is already widely used in the oil industry for Enhanced Oil Recovery (EOR) from mature oilfields. The third is coal seam storage. This involves injecting CO2 into deep coal seams no longer able to be mined. There it displaces other gases, such as methane. The displacement effect means that coal seam CO2 injection could be most effective as part of the commercial production of coal seam methane (also known as coal bed methane), an increasingly important and relatively new energy source.
The geosequestration process mimics a natural geological trapping process. Hydrocarbons such as oil and natural gas have been naturally trapped in porous underground sedimentary rocks for millions of years. Safe long-term carbon storage of CO2 has been demonstrated by the oil and gas industries for more than 40 years. At the Sleipner offshore natural gas production platform in Norway, every year since 1996 more than one million tonnes of CO2 has been transported by pipeline and safely stored deep under the seabed.
Of course, the geosequestration process does not end when the CO2 is successfully stored underground. Sites are carefully monitored, both during and long after the CO2 is injected underground. Technologies and protocols for monitoring and verification that were originally developed by the oil, gas and waste storage industries are being used to track the CO2 migration within porous rock formations and ensure that the injected CO2 remains trapped in their reservoirs.
Current CO2 storage projects such as the CO2CRC Otway project in Australia are developing and demonstrating sophisticated monitoring and verification techniques to confirm the safety and effectiveness of CO2 storage, and understand how the CO2 behaves in the storage site.
Emerging Sequestration
The underground storage of CO2 has been successfully undertaken on a commercial scale for decades. New research breakthroughs are opening up the possibility of alternative methods for managing carbon dioxide emissions that treat it as a valuable industrial input.
Like other plant life, algae have the ability to consume and capture CO2. The use of algae to capture CO2 emissions is being explored in projects around the world. Basically they involve CO2 being added to water to create biocarbonates which the algae feed on when exposed to sunlight for photosynthesis. After the algae matures it can be harvested for use in agriculture or burnt as a biofuel.
Carbon mineralisation has the advantage of storing CO2 by converting it to solid stable minerals, such as limestone, that can be stored without risk of releasing carbon into the atmosphere.
The process of carbon mineralisation is a natural one that occurs over thousands of years, but it can be accelerated by reacting CO2 at high concentrations with silicate oxide minerals to form magnesium carbonates.
While the process is easily achieved in the lab, commercial scale carbon mineralisation for storing CO2 is still at an early stage of development. A planned commercial project in the U.S. using technology from the Skyonic Corporation, involves mineralising CO2 flue emissions as sodium bicarbonate – baking soda.
The U.S. company Carbon Sciences has developed an enzyme-based technology which it claims could be used to recycle CO2 emissions into gasoline and other portable fuels. The process uses CO2 as a source of carbon and water as a source of hydrogen, to produce hydrocarbons, which are the building blocks for fuel. [PDF]