Phosphorus in agricultural soils : drivers of its distribution at the global scale

© 2017 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 23(2017), 8 vom: 09. Aug., Seite 3418-3432
1. Verfasser: Ringeval, Bruno (VerfasserIn)
Weitere Verfasser: Augusto, Laurent, Monod, Hervé, van Apeldoorn, Dirk, Bouwman, Lex, Yang, Xiaojuan, Achat, David L, Chini, Louise P, Van Oost, Kristof, Guenet, Bertrand, Wang, Rong, Decharme, Bertrand, Nesme, Thomas, Pellerin, Sylvain
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2017
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article agricultural soils biogeochemical cycles global scale modelling phosphorus Soil Phosphorus 27YLU75U4W
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520 |a Phosphorus (P) availability in soils limits crop yields in many regions of the World, while excess of soil P triggers aquatic eutrophication in other regions. Numerous processes drive the global spatial distribution of P in agricultural soils, but their relative roles remain unclear. Here, we combined several global data sets describing these drivers with a soil P dynamics model to simulate the distribution of P in agricultural soils and to assess the contributions of the different drivers at the global scale. We analysed both the labile inorganic P (PILAB ), a proxy of the pool involved in plant nutrition and the total soil P (PTOT ). We found that the soil biogeochemical background corresponding to P inherited from natural soils at the conversion to agriculture (BIOG) and farming practices (FARM) were the main drivers of the spatial variability in cropland soil P content but that their contribution varied between PTOT vs. PILAB . When the spatial variability was computed between grid cells at half-degree resolution, we found that almost all of the PTOT spatial variability could be explained by BIOG, while BIOG and FARM explained 38% and 63% of PILAB spatial variability, respectively. Our work also showed that the driver contribution was sensitive to the spatial scale characterizing the variability (grid cell vs. continent) and to the region of interest (global vs. tropics for instance). In particular, the heterogeneity of farming practices between continents was large enough to make FARM contribute to the variability in PTOT at that scale. We thus demonstrated how the different drivers were combined to explain the global distribution of agricultural soil P. Our study is also a promising approach to investigate the potential effect of P as a limiting factor for agroecosystems at the global scale 
650 4 |a Journal Article 
650 4 |a agricultural soils 
650 4 |a biogeochemical cycles 
650 4 |a global scale 
650 4 |a modelling 
650 4 |a phosphorus 
650 7 |a Soil  |2 NLM 
650 7 |a Phosphorus  |2 NLM 
650 7 |a 27YLU75U4W  |2 NLM 
700 1 |a Augusto, Laurent  |e verfasserin  |4 aut 
700 1 |a Monod, Hervé  |e verfasserin  |4 aut 
700 1 |a van Apeldoorn, Dirk  |e verfasserin  |4 aut 
700 1 |a Bouwman, Lex  |e verfasserin  |4 aut 
700 1 |a Yang, Xiaojuan  |e verfasserin  |4 aut 
700 1 |a Achat, David L  |e verfasserin  |4 aut 
700 1 |a Chini, Louise P  |e verfasserin  |4 aut 
700 1 |a Van Oost, Kristof  |e verfasserin  |4 aut 
700 1 |a Guenet, Bertrand  |e verfasserin  |4 aut 
700 1 |a Wang, Rong  |e verfasserin  |4 aut 
700 1 |a Decharme, Bertrand  |e verfasserin  |4 aut 
700 1 |a Nesme, Thomas  |e verfasserin  |4 aut 
700 1 |a Pellerin, Sylvain  |e verfasserin  |4 aut 
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