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In a phosphate transfer reaction, a phosphate group is transferred from a phosphate group donor molecule to a phosphate group acceptor molecule.
When the plant or animal dies, it decays, and the organic phosphate is returned to the soil. Within the soil, organic forms of phosphate can be made available to plants by bacteria that break down organic matter to inorganic forms of phosphorus. This process is known as mineralisation.
Phosphates exist in three forms: orthophosphate, metaphosphate (or polyphosphate) and organically-bound phosphate; each compound contains phosphorous in a different chemical arrangement.
The chemical formula of Phosphate is PO43-. Phosphate contains one Phosphorus (P) atom and four Oxygen (O) atoms. In which one central Phosphorus (P) atom is surrounded by four Oxygen (O) atoms. It forms an ionic bond between these 2 atoms.
In serum, phosphate exists in two forms, dihydrogen phosphate (H2PO4) and its salt, mono-hydrogen phosphate (HPO4). The relationship between these two can be determined by the Henderson-Hasselbalch equation. At the physiologic pH of 7.40, the pK of H2PO4 is 6.8 and the ratio of HPO4 to H2PO4 is .