The world’s nations are nowhere near to meeting the global Paris Agreement’s goals on climate change of holding global temperature increases to 2C compared to nineteenth-century averages, much less its more aspirational goal of holding temperatures to a 1.5C rise.
The most recent Emissions Gap Report from the United Nations Environment Program notes “global greenhouse gas emissions show no signs of peaking”. According to another study, the chance that humans can limit warming to no more than 2C by 2100 is no more than 5%, and it’s likely that temperatures will rise somewhere between 2.6 and 3.7C by the end of the century.
These foreboding trends have led to an increasing focus on ways to remove carbon dioxide from the atmosphere. Among the methods being explored is the use of the ocean to absorb and/or store carbon by adding crushed rocks or other sources of alkalinity to react with CO2 in seawater, ultimately consuming atmospheric CO2.
Could this type of large-scale carbon dioxide removal work? A closer look illustrates the potential environmental trade-offs of deploying marine carbon dioxide removal and the complex technical, economic and international governance issues it raises.
Land versus ocean carbon capture and storage
We and other researchers see the ocean as a logical place to look for additional carbon dioxide removal opportunities since it currently passively absorbs about 10 gigatons (10,000,000,000 tons) of CO2 per year or about one-quarter of the world’s annual emissions. In addition, the oceans contain vastly more carbon than the atmosphere, soils, plants and animals combined, and may have the potential to store trillions of tons more.
The latest report from the Intergovernmental Panel on Climate Change focused heavily on land-based methods for carbon capture and storage. One prominent technique is called bioenergy with carbon capture and storage, BECCS, where plant biomass would be burned to produce usable energy and the resulting CO2 is pumped underground.
However, there are a number of concerns about the potential negative impacts of large-scale deployment of BECCS and other land-plant-based methods, notably the worry that huge amounts of agricultural land would be diverted to grow dedicated crops. This could reduce access of low-income populations to food, place demands on water and have serious negative impacts on biodiversity due to ecosystem disruption.
Speeding up geochemistry
Perhaps the best-known – and at times, controversial – method for marine carbon dioxide removal is stimulating photosynthesis to increase CO2 absorption. For example, in regions where marine plant growth is limited by iron, this element can be added to enhance CO2 uptake and carbon storage where at least some of the biomass carbon formed eventually sinks to and is buried in the ocean floor. Other approaches include restoring, adding or culturing marine plants or microbes, such as Blue Carbon.
Another technique being considered is to try to accelerate the chemical reaction of CO2 with common rock minerals, a natural process known as mineral weathering. When rain reacts with alkaline rocks and CO2, there’s a chemical reaction, which can be catalysed by biological activity in soils, that converts the CO2 to dissolved mineral bicarbonate and carbonate ions which then typically run off into the ocean. Mineral weathering plays a major role in removing excess atmospheric CO2, but only on geologic time scales – 100,000 years or more.
The natural process of mineral weathering starts with rain which absorbs carbon dioxide from the air and then reacts with rock and biota in soils, forming dissolved mineral bicarbonate and a much smaller quantity of carbonate ions. These then run off into the ocean where the carbon is stored in these forms for many millennia before precipitating to the ocean floor as carbonate minerals. The idea of enhanced weathering is to greatly speed up this process by adding crushed rocks or other sources of alkalinity to react with CO2 in seawater, ultimately consuming atmospheric CO2 and adding it as dissolved mineral bicarbonate and carbonate to the already very large reservoir of these compounds in the ocean.
Various ways to accelerate mineral weathering and ocean carbon storage that have been proposed include adding to surface waters finely ground alkaline minerals or adding common, industrially produced alkaline chemicals, such as quicklime (CaO), calcium hydroxide (Ca(OH)2), and lye or caustic soda (NaOH). Once added to the ocean, these compounds react with excess CO2 in seawater and air, principally forming stable, dissolved mineral bicarbonate, thus removing and sequestering CO2.
Such ocean alkalization could be achieved via distribution from shore or by ships. Another proposal is to manufacture alkalinity at sea using local marine energy sources: for example, employing electricity derived from the ocean’s very significant vertical temperature gradient. Reacting waste CO2 with minerals on shore and then pumping the resulting dissolved alkaline material into the ocean is also an option. All of the preceding would simply add to the already vast bicarbonate and carbonate reservoir in the ocean.
An additional benefit of ocean alkalization is that it also helps counter ocean acidification, the “other CO2 problem” stemming from the ocean’s absorption of excess CO2 from the air. Acidification can interfere with the ability of calcifying organisms, such as oysters, clams and corals to construct their skeletons or shells, as well as impact other pH-sensitive marine biogeochemical processes.
What we don’t know
The actual practical capacity of ocean alkalization to counter climate change and acidification remains uncertain.
Considering the logistics, cost and impacts of extracting or manufacturing alkalinity and dispersing it, studies estimate that air CO2 drawdowns of perhaps 30 parts per million or less might be realistic. This would be helpful given that the level of CO2 in preindustrial times was 260-270 parts per million and is now 410 parts per million.
We calculate a global drawdown of atmospheric CO2 by 30 parts per million would require near-zero emissions from human activities, plus the removal and storage of some 470 gigatons of CO2. To achieve this, a minimum of roughly 500 gigatons of rock would need to be used to generate the required alkalinity. Current global rock extraction is on the order of 50 gigatons per year, so holding other rock uses steady while increasing this extraction rate by 50 percent could theoretically allow us to achieve the drawdown in 20 years. This obviously needs to be tested at vastly smaller scales to determine what global capacity and rates might be realisable.
Nor is this just a matter of alkalinity production; there are potential negative impacts of ocean alkalization on marine ecosystems that need to be considered. In addition to the effects of pH and alkalinity elevation (either instantaneous or gradual), alkalinity addition would likely carry with it other elements or compounds, such as trace metals and silica, that can also affect marine biogeochemistry. Little research has been conducted on these points, but the results so far generally find no or positive effects on marine life. Further investigation is needed to fully understand the environmental and ecological consequences, including conducting small and medium-sized field trials.
Any deployment would need to be subjected to strict monitoring requirements to assess both the environmental benefits and well as the negative impacts of large-scale deployment. Some measure of confidence in the use of ocean alkalization might be found in the fact that natural mineral weathering and alkalinity delivery to the ocean has naturally occurred for billions of years (currently at the rate of about 1 gigaton of CO2 consumed and stored per year), apparently with the marine ecosystem well adapted to, if not requiring, this input. Nevertheless, the possibility of significantly and safely scaling up this natural process requires further research.
At a legal level, countries would need to address international governance issues associated with this approach. Presumably, the Paris Agreement would be one of the regimes involved given its focus on addressing climate change. Any role ocean alkalinity could play in countries’ pledges to mitigate emissions would require provisions that mandate assessment of potential impacts of deployment. The Paris Agreement could facilitate this given its references in various provisions to the need to assess the impacts of response measures in the context of ecosystems, sustainability, development and human rights.
Ocean-focused regimes such as the Convention on the Prevention of Marine Pollution by Dumping of Wastes and Other Matter and the Law of the Sea Convention, and its Protocol, might also seek to be engaged in assessment and regulation, as well as the Convention on Biological Diversity. Coordinating the potential interventions of all of these regimes’ responses would be another challenge posed by deployment of ocean alkalinity, as would the many other carbon dioxide removal approaches that could have transboundary impacts.
The spectre of potentially catastrophic climate change by the end of the century has stimulated interest in an array of new technological options to remove CO2 from the ocean and atmosphere at large scale. But they could also pose risks of their own. Adding alkaline materials to speed up mineral weathering is one such approach that deserves serious consideration, though only after thorough scrutiny.
This article is republished from The Conversation