“…Thus, soil bioavailable P could be defined as the potential supply of available P released from the soil by the rhizospheric processes of plant roots and microbes (Comerford, ). Four potential mechanisms of P acquisition by plants can be generalised: (a) root interception and diffusion of the soluble inorganic P pool that is easily available to the plants via root morphology modifications and mycorrhizal formations (Bolan, ), (b) organic acid complexation and dissolution of the active inorganic P pool that sorb onto clay particles or weakly bind to iron (Fe) or aluminium (Al) precipitates through organic acid exudation (Giles et al, ; Grinsted, Hedley, White, & Nye, ), (c) enzymatic hydrolysis of the labile organic P pool by phosphatase and phytase exudation (Fatemi, Fernandez, Simon, & Dail, ; Giles et al, ), and (d) H + /OH − /HCO 3 − extrusion of the occluded inorganic P pool that is used with difficulty by plants through H + /OH − /HCO 3 − exudation (Hedley et al, ; Latati et al, ) in the rhizosphere by plant roots and soil microbes. Deluca et al () proposed an extraction method that emulates the above four mechanisms through the use of four extractions (CaCl 2 , citric acid, phytase and phosphatase, and HCl) in parallel along a P lability to recalcitrant gradient and defined the four forms of bioavailable soil P as CaCl 2 ‐P, citric‐P, enzyme‐P and HCl‐P, respectively.…”