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Sulfation reactions are thought to be rate-limited by endogenous sulfate concentrations.
Rainfall over the southwestern United States contains relatively high sulfate concentrations because of sulfate-bearing particles that have been blown into the atmosphere from desert soils.
Such low pH values and increased nitrate and sulfate concentrations also are found in the rains of western Europe and other industrialized regions of the world.
Low sulfate concentrations may cause damage.
Increased sulfate concentrations were detected at all weathering features.
Unexpectedly, lower sulfate concentrations had no effect on Se removal.
Sulfate concentrations vary little with depth during fall, when the sediment pore waters are mostly suboxic.
This phenomenon was used to calibrate sulfate concentrations in the Archean ocean [51].
The low sulfur isotopic fractionation is interpreted as indication for sulfate concentrations <200 µM.
Sulfate concentrations remained in the 524 535 µM range throughout the water column.
Sulfate concentrations of 0.5 4.5 mM have been suggested for the Mesoproterozoic ocean [101].
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