Olivine Weathering Can Reverse Global Warming in Our Lifetime
worksinprogress.co
worksinprogress.co
This is something that can be studied as marine layers already contain many examples of both slow and rapid depositation.
One example of grand scale carbonate deposits are the Bunda cliffs - 210 kilometres in length, 120 metres in height, some 20-30 km in width (the material of the cliff face extends inland).
(That's a valid point, however, about the expected hazards to the people running the milling machines. Maybe there are good ways to mitigate that? Maybe wet milling minimizes the problem? The author doesn't say.)
Silt can be incredibly destructive. Before hydraulic (gold) mining in the Sierras, the Sacramento river was navigable all the way to.... um, Sacramento, and the waters of San Francisco Bay were crystal clear, and carpeted with oysters. Silt washed down 150-ish years ago is still gunking up the entire ecosystem.
This is an intriguing idea, and global warming is a planetary emergency - so some degree of localized destruction may be a reasonable trade-off - but the author gets poor marks from me for leaving obvious negative externalities out of the article.
The solution would be to keep thr particle size larger, at lower efficiency.