Towards a global model for soil inorganic phosphorus dynamics: dependence of exchange kinetics and soil bioavailability on soil physicochemical properties

Ying‐ping Wang (1) , Yuanyuan Huang (1) , Laurent Augusto (2) , Daniel S Goll (3, 4) , Julian Helfenstein (5) , Enqing Hou (6)

1 CSIRO Marine and Atmospheric Research [Aspendale]
2 UMR ISPA - Interactions Sol Plante Atmosphère
3 LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
4 MOSAIC - Modélisation des Surfaces et Interfaces Continentales
5 agroscope
6 Guangzhou University

The representation of phosphorus cycling in global land models remains quite simplistic, particularly on soil inorganic phosphorus. For example, sorption and desorption remain unresolved and their dependence on soil physical and chemical properties is ignored. Empirical parameter values are usually based on expert knowledge or data from few sites with debatable global representativeness in most global land models. To overcome these issues, we compiled from data of inorganic soil phosphorus (P) fractions and calculated the fraction of added P remaining in soil solution over time of 147 soil samples to optimize three parameters in a model of soil inorganic P dynamics. The calibrated model performed well (r2>0.7 for 122 soil samples). Model parameters vary by several orders of magnitude, and correlate with soil P fractions of different inorganic pools, soil organic carbon and oxalate extractable metal oxide concentrations among the soil samples. The modelled bioavailability of soil P depends on, not only, the desorption rates of labile and sorbed pool, inorganic phosphorus fractions, the slope of P sorbed against solution P concentration, but also on the ability of biological uptake to deplete solution P concentration and the time scale. The model together with the empirical relationships of model parameters on soil properties can be used to quantify bioavailability of soil inorganic P on various timescale especially when coupled within global land models.

Mots clés: phosphorus fractions; global modelling; Hedley fractionation; isotopic exchange kinetics; sorption; desorption; available phosphorus

Domaines: Océan, Atmosphère; Interfaces continentales, environnement

Ying‐ping Wang, Yuanyuan Huang, Laurent Augusto, Daniel S Goll, Julian Helfenstein, et al.. Towards a global model for soil inorganic phosphorus dynamics: dependence of exchange kinetics and soil bioavailability on soil physicochemical properties. Global Biogeochemical Cycles, 2022, 36 (3), pp.e2021GB007061. ⟨10.1029/2021GB007061⟩. ⟨hal-03607493⟩