The phosphorus status of German cropland—An inventory of top- and subsoils

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Abstract

Background: In search for more sustainable crop production, the subsoil has recently come into focus as considerable reservoir of nutrients and water. Aims: Dimensions of subsoil phosphorus (P) reserves are yet largely unknown but crucial for identifying regions suitable to include subsoil into sustainable management strategies. Methods: We analyzed stocks of total and plant-available (calcium acetate lactate-extractable) P in 96 representative soil profiles of German arable land down to 1 m depth. Results: We found that the German arable soils stored, on average, 8 t ha−1 of total P, of which nearly 500 kg ha−1 were readily plant-available. Notably, one third of plant-available P was located below the plow layer and one fifth even at depths below 0.5 m. The depth gradients of plant-available P stocks were affected more by major reference soil group than by texture. Generally, Chernozem but also Anthrosol, Gleysol and Fluvisol exhibited the largest P stocks in German cropland. The contribution of plant-available P to total P stocks was larger in sandy and extremely acidic (pH < 4.5) soils compared with more fine-grained and slightly acidic to alkaline soils, possibly because fertilization compensated for overall lower total P stocks at these sites. Generally, the more P was stored in topsoils, the more P was stored also in subsoils. Conclusions: A hypothetical crop utilization of 10% from plant-available P stocks and 0.1% from total P stocks from shallow subsoil could compensate for P fertilization by ca. 8 kg ha−1, but the rate of plant-available P replenishment in subsoil likely remains the crucial factor for the role of subsoil P stocks in crop nutrition. Generally, the large P reserves found in subsoil could act as an ‘insurance' system for crops.

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Gocke, M. I., Don, A., Heidkamp, A., Schneider, F., & Amelung, W. (2021). The phosphorus status of German cropland—An inventory of top- and subsoils. Journal of Plant Nutrition and Soil Science, 184(1), 51–64. https://doi.org/10.1002/jpln.202000127

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