
Take: How Much CO₂ Can Enhanced Weathering Really Remove? - Derry
Take on a podcast episode from Reviewer 2 does geoengineering, originally published Mon, 28 Se. Listen: https://podcasters.spotify.com/pod/show/reviewer2geoengineering/episodes/How-Much-CO-Can-Enhanced-Weathering-Really-Remove----Derry-e3pgntl TL;DR Derry’s whole-system argument: shallow-soil cation depletion (top 10–30 cm) measures the first step, not alkalinity export. Direct challenge to current ERW measurement, reporting, and verification (MRV). Three sinks consume alkalinity downstream: ion exchange in acidic soils, secondary clay precipitation (generates acidity), carbonate precipitation. “Not delayed, it’s been consumed.” Water budget check: ~250 mm/yr runoff in US corn belt would need 25–30 mmol/L alkalinity to move 5 t CO₂/ha/yr; real streams run 1–3. Useful framing. Natural basalt catchments max out near 1 t CO₂/ha/yr (wet tropics), typically ~0.2. Global basalt weathering ~0.1–0.15 Gt CO₂/yr. First time I’ve seen this benchmark set against ERW claims. Host tone is snarky; guest is measured and explicitly open to rebuttal. Take the substance, discount the wrapper. Andrew of Reviewer 2 does geoengineering hosts Louis Derry, Cornell geochemist (30 years, also affiliated with IPGP Paris), on a new Nature paper with Kate Maher and Oliver Chadwick arguing that critical-zone processes cap alkalinity export from basaltic systems. The episode is essentially a mechanistic case for why enhanced rock weathering (ERW) removal claims of 5–10 t CO₂/ha/yr are physically implausible in row-crop agriculture. ...








