|
|
|
|
|
by pfdietz
1073 days ago
|
|
Counterions like magnesium are quite abundant. After all, this is how CO2 will be drawn down if we do nothing (but it will take hundreds of thousands of years.) There has been much work on exploiting the more reactive silicates, like olivine, to fix CO2. The volumes of rock involved are large, but there's a lot of silicates out there. |
|