Abstract
THE availability to plants of molybdate in some acidic soils may be increased by raising the pH. This behaviour of molybdate is analogous to that of phosphate, and suggests a study of its compounds with iron and aluminium, which are presumably responsible for holding molybdate in an insoluble form.
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References
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JONES, L., MILNE, A. Aluminium Molybdate and its Formation in Clay Minerals. Nature 178, 1115 (1956). https://doi.org/10.1038/1781115a0
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DOI: https://doi.org/10.1038/1781115a0
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