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Agricultural activities increase silicate weathering.
Wallmann, K. et al. Silicate weathering in anoxic marine sediments.
Silicate weathering normally results in the elevation of Na and K concentration in groundwater.
Mayback (1987) reported that the Na/Cl >1 is an indication of the origin of Na from the silicate weathering.
The dissolved silica lacks representations in the factor loadings resembles that fluoride is less influenced by the silicate weathering.
In the presence of a biosphere, burial of organic carbon also contributes to atmospheric carbon sequestration in addition to silicate weathering.
We report a direct linkage between photosynthate-energy fluxes from trees to EM and AM mycorrhizal mycelium and rates of calcium silicate weathering.
West, A. J., Galy, A. & Bickle, M. Tectonic and climatic controls on silicate weathering.
Meysman, F. J. R. & Montserrat, F. Negative emissions via enhanced silicate weathering in coastal environments.
However, we note that in many modern settings silicate weathering is supply-limited33.
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"However, atmospheric carbon dioxide levels aren't changing because the Earth has had time to respond via increased silicate-weathering rates.
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