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Abstract Enhanced weathering, adding crushed silicate minerals to soils, is being explored as a way to draw down atmospheric carbon dioxide, but its effects on soil organic carbon remain uncertain. We show that olivine amendments change soil carbon cycling depending on time and on labile carbon availability. In a 55-week soil microcosm experiment, adding olivine alone reduces total soil organic carbon.
As a journalist, you can create a free Muck Rack account to customize your profile, list your contact preferences, and upload a portfolio of your best work.
