Articles | Volume 13, issue 12
https://doi.org/10.5194/essd-13-5831-2021
https://doi.org/10.5194/essd-13-5831-2021
Data description paper
 | 
20 Dec 2021
Data description paper |  | 20 Dec 2021

Global patterns and drivers of soil total phosphorus concentration

Xianjin He, Laurent Augusto, Daniel S. Goll, Bruno Ringeval, Yingping Wang, Julian Helfenstein, Yuanyuan Huang, Kailiang Yu, Zhiqiang Wang, Yongchuan Yang, and Enqing Hou

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Cited articles

Achat, D. L., Augusto, L., Gallet-Budynek, A., and Loustau, D.: Future challenges in coupled C-N-P cycle models for terrestrial ecosystems under global change: a review, Biogeochemistry, 131, 173–202, https://doi.org/10.1007/s10533-016-0274-9, 2016a. 
Achat, D. L., Pousse, N., Nicolas, M., Brédoire, F., and Augusto, L.: Soil properties controlling inorganic phosphorus availability: general results from a national forest network and a global compilation of the literature, Biogeochemistry, 127, 255–272, https://doi.org/10.1007/s10533-015-0178-0, 2016b. 
Adams, J., Tipping, E., Thacker, S. A., and Quinton, J. N.: Phosphorus, carbon and nitrogen concentrations in UK soil mineral fractions, 2013–2014, NERC Environmental Information Data Centre, https://doi.org/10.5285/e6e9a85c-b537-4110-899f-2c1498bc826c, 2020. 
Alewell, C., Ringeval, B., Ballabio, C., Robinson, D. A., Panagos, P., and Borrelli, P.: Global phosphorus shortage will be aggravated by soil erosion, Nat. Commun., 11, 4546, https://doi.org/10.1038/s41467-020-18326-7, 2020. 
Amberger, A.: Pflanzenernährung. Ökologische und physiologische Grundlagen, Dynamik und Stoffwechsel der Nährelemente, 4th edn., Eugen Ulmer, Stuttgart, Germany, 1996 (in German). 
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Our database of globally distributed natural soil total P (STP) concentration showed concentration ranged from 1.4 to 9630.0 (mean 570.0) mg kg−1. Global predictions of STP concentration increased with latitude. Global STP stocks (excluding Antarctica) were estimated to be 26.8 and 62.2 Pg in the topsoil and subsoil, respectively. Our global map of STP concentration can be used to constrain Earth system models representing the P cycle and to inform quantification of global soil P availability.
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