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Regional potential of coastal ocean alkalinization with olivine within 100 years
The spreading of crushed olivine-rich rocks in coastal seas to accelerate weathering reactions sequesters atmospheric CO _2 and reduces atmospheric CO _2 concentrations. Their weathering rates depend on different factors, including temperature and the reaction surface area. Therefore, this study investigates the variations in olivine-based enhanced weathering rates across 13 regional coasts worldwide. In addition, it assesses the CO _2 sequestration within 100 years and evaluates the maximum net-sequestration potential based on varying environmental conditions. Simulations were conducted using the geochemical thermodynamic equilibrium modeling software PHREEQC. A sensitivity analysis was performed, exploring various combinations of influencing parameters, including grain size, seawater temperature, and chemistry. The findings reveal significant variation in CO _2 sequestration, ranging from 0.13 to 0.94 metric tons (t) of CO _2 per ton of distributed olivine-rich rocks over 100 years. Warmer coastal regions exhibit higher CO _2 sequestration capacities than temperate regions, with a difference of 0.4 t CO _2 /t olivine distributed. Sensitivity analysis shows that smaller grain sizes (10 µ m) exhibit higher net CO _2 sequestration rates (0.87 t/t) in olivine-based enhanced weathering across all conditions, attributed to their larger reactive surface area. However, in warmer seawater temperatures, olivine with slightly larger grain sizes (50 and 100 µ m) displays still larger net CO _2 sequestration rates (0.97 and 0.92 t/t), optimizing the efficiency of CO _2 sequestration while reducing grinding energy requirements. While relying on a simplified sensitivity analysis that does not capture the full complexity of real-world environmental dynamics, this study contributes to understanding the variability and optimization of enhanced weathering for CO _2 sequestration, supporting its potential as a sustainable CO _2 removal strategy.
Regional potential of coastal ocean alkalinization with olivine within 100 years
The spreading of crushed olivine-rich rocks in coastal seas to accelerate weathering reactions sequesters atmospheric CO _2 and reduces atmospheric CO _2 concentrations. Their weathering rates depend on different factors, including temperature and the reaction surface area. Therefore, this study investigates the variations in olivine-based enhanced weathering rates across 13 regional coasts worldwide. In addition, it assesses the CO _2 sequestration within 100 years and evaluates the maximum net-sequestration potential based on varying environmental conditions. Simulations were conducted using the geochemical thermodynamic equilibrium modeling software PHREEQC. A sensitivity analysis was performed, exploring various combinations of influencing parameters, including grain size, seawater temperature, and chemistry. The findings reveal significant variation in CO _2 sequestration, ranging from 0.13 to 0.94 metric tons (t) of CO _2 per ton of distributed olivine-rich rocks over 100 years. Warmer coastal regions exhibit higher CO _2 sequestration capacities than temperate regions, with a difference of 0.4 t CO _2 /t olivine distributed. Sensitivity analysis shows that smaller grain sizes (10 µ m) exhibit higher net CO _2 sequestration rates (0.87 t/t) in olivine-based enhanced weathering across all conditions, attributed to their larger reactive surface area. However, in warmer seawater temperatures, olivine with slightly larger grain sizes (50 and 100 µ m) displays still larger net CO _2 sequestration rates (0.97 and 0.92 t/t), optimizing the efficiency of CO _2 sequestration while reducing grinding energy requirements. While relying on a simplified sensitivity analysis that does not capture the full complexity of real-world environmental dynamics, this study contributes to understanding the variability and optimization of enhanced weathering for CO _2 sequestration, supporting its potential as a sustainable CO _2 removal strategy.
Regional potential of coastal ocean alkalinization with olivine within 100 years
Murugan Ramasamy (author) / Thorben Amann (author) / Nils Moosdorf (author)
2024
Article (Journal)
Electronic Resource
Unknown
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