“…To date, the potential of enhanced weathering for removing atmospheric CO 2 has principally been estimated using modeling studies (e.g., Renforth, 2012;Taylor et al, 2016;Beerling et al, 2020;Bullock et al, 2021), or based on results from small-scale mesocosm or laboratory experiments (e.g., Renforth et al, 2015;Amann et al, 2020;Kelland et al, 2020;Pogge von Strandmann et al, 2021). Most mesocosm and laboratory studies to date have focused on amending soils with relatively fast weathering silicate minerals, notably olivine, or fast weathering silicate rocks, such as dunite that contains a high proportion of olivine.…”