Soil organic matter (SOM) is unevenly distributed in arable fields in undulated landscapes, but the chemical composition resulting from their turnover, transport and deposition processes is insufficiently known. Therefore, we aimed at disclosing the molecular-chemical composition of SOM in four different catenae at shoulderslope, backslope and footslope positions in arable fields in the Baltic Sea catchment, Europe. The backslope positions always had the lowest organic C-contents (C_org) (1.6…11.8 g·kg⁻¹) and C-stocks (3.8…8.5 kg·m⁻²) compared to the shoulderslopes and footslopes (1.7…17.7 g·C_org·kg⁻¹, 5.4…15 kg·C_org·m⁻²). In the SOM-poor backslope positions, the organic matter was characterized by relatively high proportions of carbohydrates, phenols + lignin monomers, alkylaromatic compounds, N-compounds and amides, indicating intensive microbial decomposition. By contrast, the footslopes had the largest C_org-contents (9.3…16.5 g·kg⁻¹) and C-stocks (8.9…15 kg·m⁻²) in the catenae and particular enrichments in lipids, lignin dimers, sterols and free fatty acids. These relatively stabile SOM compound classes are interpreted as leftovers from erosive downslope transport and concurrent microbial decomposition, e.g., they are pronounced at backslope positions, followed by restricted microbial decomposition. This heterogeneous SOM distribution calls for an adapted soil management that reduces erosion and places amendments to field areas, such as the shoulderslope and backslope.

Although lipids are involved in diverse soil processes and affect various soil properties, the contribution of rhizodeposits and the root zone to lipid concentrations and distributions in soils is unknown. For the first time, we determined the concentrations of alkanoic acids, n-alkanes and n-alkenes in root zone leachates and roots of maize and potato using gas chromatography/mass spectrometry (GC/MS). In total, the lipid concentrations of leachates were 100 μg g⁻¹ (maize) and 17 μg g⁻¹ (potato). The saturated n-alkanoic acids, ranging from n-C₁₄ to n-C₂₈ and having the maximum at n-C₂₂ (maize) and at n-C₁₆ (potato), were more abundant than the other compounds. Maize leachates had more alkanes (20 μg g⁻¹) than potato leachates (3.1 μg g⁻¹), but the members of the homologues were nearly the same. Comparison of these distributions with data for roots, microorganisms and soil indicated that the lipids in the leachates from the root zone mainly originated from abrasion of fine roots, rhizodeposits and rhizosphere microorganisms.