“…The availability of P is controlled, mainly, by the partition of its chemical fractions according to their lability in the soil (Larsen, 1967): labile in the form of P-H2O and P-Al, and non-labile in the form of P-Fe and P-Ca (Santos and Conceição, 2018;Pereira et al, 2020). Furthermore, it is known that in soils with a more acidic pH, the P fixation process occurs, preferably, together with the Fe (P-Fe) and Al (P-Al) ions, and, in more alkaline soils, the precipitation, mainly with the Ca ion (P-Ca) (Medeiros et al, 2021). Therefore, soil pH is a determining attribute in the dynamics of the availability of this macronutrient for plants (Gatiboni et al, 2008;Rosa et al, 2018) since acidity influences the load balance of solid soil particles, consequently in the sorption process of this anion together with colloids (Vasconcelos et al, 2022).…”