Years of researchers looking into carbon sequestration have concluded two things:
1. It’s far better to reduce emissions than rely on sequestration to avoid climate catastrophe
2. Ocean-based sequestration is more efficient than direct air capture.
A team of researchers have found a way to get container ships to help with sequestration of carbon into the ocean by using an accelerated natural process. It’s well known that modern fossil-fuel powered shipping is very bad for the planet so the researchers wondered what if we could leverage the movement of ships on the water to spread limestone over greater distances? They modelled it out and this approach of using ships as a way to spread the carbon sequestration method is quite efficient and better than a stationary setup.
Calcium carbonate dissolution is the dominant negative feedback in the ocean for neutralizing the acidity from rising atmospheric carbon dioxide. Mimicking this natural process, the accelerated weathering of limestone (AWL) can store carbon as bicarbonate in the ocean for tens of thousands of years. Here, we evaluate the potential of AWL on ships as a carbon sequestration approach. We show a successful prediction of laboratory measurements using a model that includes the most recent calcite dissolution kinetics in seawater. When simulated along a Pacific shipping lane in the Estimating the Circulation and Climate of the Ocean–Darwin ocean–general circulation model, surface alkalinity and dissolved inorganic carbon increase by <1.4% after 10 years of continuous operation, leaving a small pH and partial pressure of carbon dioxide impact to the ocean while reducing 50% carbon dioxide emission in maritime transportation.
