I think that not everybody realizes that some 300 million tons of CO2 are 
captured every year by the weathering of basic silicates, notably the most 
common one, olivine. To demonstrate this, the diagram below shows the 
analytical data of some 20 spring water samples in olivine rocks in Turkey. It 
shows what happens when rain falls on soils on top of olivine rocks. The 
rainwater contains essentially only some CO2 and has a pH in the order of 6. 
Then it penetrates the soil, which has much higher CO2 concentrations in the 
soil atmosphere than in the atmosphere above. Dead plant material is decaying, 
the soil fauna is breathing, both releasing CO2, so the CO2 concentration of 
the soil atmosphere is often hundred times or more higher than in the 
atmosphere. The water equilibrates with this high CO2 concentration. Then it 
seeps into the rock, and reacts with it, releasing magnesium to the solution, 
and the pH rises to values around 7.5 to 8.5. This weathering reaction can be 
written as

Mg2SiO4 + 4 CO2 + 4 H2O  --> 2 Mg2+ + 4 HCO3- + H4SiO4 (so the CO2 is captured 
as bicarbonate in solution).

At some point this water is emitted again as a spring. This spring water is 
very healthy, and we often had to wait in line for the many people who collect 
this spring water in containers and jerrycans to bring home. Most of the water 
flows away in small brooks, and finally reaches the sea, where the calcium and 
magnesium are used by plankton, corals and shellfish to form limestones and 
dolomites, the ultimate sustainable storage of the CO2.
Just as an afterthought: so if we irrigate semi-arid land on top of olivine 
massifs, we have a cheap way to fix CO2 by increasing the number and the volume 
of springs in such rocks, Olaf Schuiling
I attach the paper in which these data were published

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[cid:[email protected]]




















   ®



Fig.1:  Concentration in meq [Ca2+ + Mg2+] in spring waters. Total carbon as mg 
CO2.
® composition of rain water.

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