Phosphorus Basics – The Phosphorus Cycle
which happens if plant available inorganic P reacts with dissolved iron, aluminum, manganese (in acid soils), or calcium (in alkaline soils) to form phosphate minerals. Mineralization and Immobilization Mineralization is the microbial conversion of organic P to H 2PO 4-or HPO 4 2-, forms of plant available P known as orthophosphates.
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As a result, treatment with inorganic acid solutions leads to layer charge reduction due to leaching of the octahedral cations and the structural degradation; all of which leads to a decrease in the cation exchange capacity. In addition, amorphous silica appeared as .