“…The metal ions can then react with CO 2 dissolved in water from the atmosphere to form extremely long-lived carbonate minerals (Power et al, 2013a). For example, peridotite reservoirs across the globe (largely containing olivine) have the potential to mineralize and sequester 10 5 -10 8 GtCO 2 (Kelemen et al, 2019), between 100 and 100,000 3 the excess CO 2 in the atmosphere (z1,000 to 1,500 GtCO 2 ) (Global Monitoring Laboratory, 2022; Lackner and Azarabadi, 2021). Natural weathering (where the breakdown of the mineral occurs However, the world's growing (Prosekov and Ivanova, 2018) and increasingly wealthy population (Hawksworth and Chan, 2015) are creating a growing need for arable land (Tilman et al, 2011), tightening the world's biomass supply (Slade et al, 2014).…”