Linking transport pathways and phosphorus distribution in a loamy soil: a case study from a North-Eastern German Stagnosol

Heterogeneous flow pathways through the soil determine the transport of dissolved and particle-bound nutritional elements like phosphorus (P) to ground and surface waters. This study was designed to understand the spatial patterns of P in agriculturally used soils and the mechanisms causing P accumulation and depletion at the centimetre scale. We conducted dye tracer experiments using Brilliant Blue on a loamy Stagnosol in North-Eastern-Germany. The plant-available P was analysed using double lactate extraction (DL-P). The plant-available P content of the topsoil was significantly higher than that of the subsoil in all three replicates (p < 0.001). The topsoil's stained areas showed significantly higher P contents than unstained areas (p < 0.05), while the opposite was found for the subsoil. The P content varied enormously across all observed soil profiles (4 to 112 mg P kg(-1) soil) and different categories of flow patterns (matrix flow, flow fingers, macropore flow, and no visible transport pathways). The P contents of these transport pathways differed significantly and followed the order: P-matrix flow > P-finger flow > P-no visible transport pathways > P-macropore flow. We conclude that P tends to accumulate along flow pathways in the topsoil in the observed fertilized and tilled mineral soil. In contrast, in the subsoil at a generally lower P level, P is depleted from the prominent macroporous flow domains.

Automated summary

Heterogeneous flow pathways through the soil determine the transport of dissolved and particle-bound nutritional elements like phosphorus (P) to ground and surface waters. This study aimed to understand the spatial patterns of P in agriculturally used soils and the mechanisms causing P accumulation and depletion at the centimeter scale. Dye tracer experiments using Brilliant Blue were conducted on a loamy Stagnosol in North-Eastern-Germany. The results showed that P tends to accumulate along flow pathways in the topsoil, while it is depleted from the macroporous flow domains in the subsoil.