Simulating the soil phosphorus dynamics of four long‐term field experiments with a novel phosphorus model

Gasser, S. Anton A. ORCIDiD
Nielsen, Kerstin
Eichler‐Löbermann, Bettina
Armbruster, Martin
Merbach, Ines
Franko, Uwe

DOI: https://doi.org/10.1111/sum.12881
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11188
Gasser, S. Anton A.; Nielsen, Kerstin; Eichler‐Löbermann, Bettina; Armbruster, Martin; Merbach, Ines; Franko, Uwe, 2023: Simulating the soil phosphorus dynamics of four long‐term field experiments with a novel phosphorus model. In: Soil Use and Management, 39, 2, 867-880, DOI: https://doi.org/10.1111/sum.12881. 
 
Nielsen, Kerstin; 2 Lebenswissenschaftliche Fakultät Institut für Agrar‐und Stadtökologische Projekte an der Humboldt‐Universität zu Berlin (IASP) Berlin Germany
Eichler‐Löbermann, Bettina; 3 Agronomy and Crop Science University of Rostock Rostock Germany
Armbruster, Martin; 4 Agricultural Analytical and Research Institute Speyer (LUFA Speyer) Speyer Germany
Merbach, Ines; 1 Helmholtz Centre for Environmental Research GmbH – UFZ Halle (Saale) Germany
Franko, Uwe; 1 Helmholtz Centre for Environmental Research GmbH – UFZ Halle (Saale) Germany

Abstract

Phosphorus is a nonrenewable resource, which is required for crop growth and to maintain high yields. The soil P cycle is very complex, and new model approaches can lead to a better understanding of those processes and further guide to research gaps. The objective of this study was to present a P‐submodel, which has been integrated in the existing Carbon Candy Balance (CCB) model that already comprises a C and N module. The P‐module is linked to the C mineralization and the associated C‐pools via the C/P ratio of fresh organic material. Besides the organic P cycling, the module implies a plant‐available P‐pool (Pav), which is in a dynamic equilibrium with the nonavailable P‐pool (Pna) that comprises the strongly sorbed and occluded P fraction. The model performance was tested and evaluated on four long‐term field experiments with mineral P fertilization, farmyard manure as organic fertilizer and control plots without fertilization. The C dynamics and the Pav dynamics were modelled with overall good results. The relative RMSE for the C was below 10% for all treatments, while the relative RMSE for Pav was below 15% for most treatments. To accommodate for the rather small variety of available P‐models, the presented CNP‐model is designed for agricultural field sites with a relatively low data input, namely air temperature, precipitation, soil properties, yields and management practices. The CNP‐model offers a low entry threshold model approach to predict the C‐N and now the P dynamics of agricultural soils.