Originally posted by workboots
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Mineralization- the amount of organic material turned into inorganic phosphorus through soil biological activity. Humic acid plays a role here creating healthy soil crumbs and food for biologicals realasing inorganic material back into a soil solution phosphorus (plant available) temp, moisture also effect speed at which OM is broken down.
Adsorption- Process in which metal ions (inorganic phosphorus or plant available) bind with other elements, this rate is influenced by ph and soil type. High ph tend to have elevated Ca and low ph elevated Al, Fe or called "sorbed phosphorus" This is where TPA gets involved and has big upside. The realses or unbinding process is called dissolution and is extreamly slow.
Out of all 3 of the phosphorus "pools" in your soil it is of my understanding that the fixed pool consisting of phosphorus that is unavailable for plant uptake and is comprised of primary minerals (insoluble inorganic phosphate compounds) and organic phosphorus compounds that do not mineralize easily would be the largest.
Second pool consists of "absorbed" phosphorus so your binded po4 and organic phosphorus that minerlizes easier.
Third and smallest would be your inorganic (plant available) phosphorus.
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