97-99% of the total P in the soil are in plant unavailable form, which may be either in the form of unavailable inorganic P like Ca-P, Fe-P, Al-P or in the form of unavailable organic P like Phytin, lecithin, glycerophosphates etc. Microorganisms solubilize unavailable inorganic P after releasing/producing organic acids that are dissolving Ca, Fe or Al bond. Sometimes same microorganisms also releasing/producing phosphatases and phytase enzymes which are mobilizing organic P after breaking the C-O-P ester bond. My question is where they spent/need more energy during mobilization or during solubilization. Why some organisms inclined to mobilize organic P and some like to solubilize inorganic P?

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