Summary
Silicon in soil solutions is present entirely as monosilicic acid and soils are capable of maintaining a steady concentration in solution despite repeated withdrawals. This concentration is always below the saturation figure of 120 ppm SiO2 and varies amongst soils of the same pH.
Both ferric and aluminium oxides adsorb monosilicic acid but among oxides of similar crystallinity, aluminium oxide is more effective than ferric oxide. When added to a soil, both ferric and aluminium oxides lowered the concentration of monosilicic acid in solution. Aluminium oxide again had the greater effect and one sample lowered the concentration of monosilicic acid from 48 to 9 ppm SiO2.
In pot experiments oats were grown in a soil to which ferric and aluminium oxides had been added and also in soils differing naturally in their content of free sesquioxides. The uptake of silica by the plants can be explained simply in terms of the concentration of silica in the soil solution and the amount of water transpired. This indicates that oats take up silica passively in the transpiration stream.
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Jones, L.H.P., Handreck, K.A. Studies of silica in the oat plant. Plant Soil 23, 79–96 (1965). https://doi.org/10.1007/BF01349120
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DOI: https://doi.org/10.1007/BF01349120