Abstract

Intensive tillage, non-diversified crop rotations and reduction in the return of organic residues to soil imply decreasing levels of soil organic carbon (SOC). Straw removal for (bio)energy production may increase in the future, given the attempts to phase out fossil energy sources. The decreasing SOC contents may deteriorate soil structure with adverse effects on soil ecosystem services. In this study, the long-term (28–36 years) effect of repeated experimentation with removal, burning or incorporation of straw was quantified at a coarse sandy and two sandy loam soils. At the end of experimentation, remolded soil was sampled and analyzed for SOC and a range of other chemical characteristics. Undisturbed soil cores were collected in the plough layer (10 cm depth) and the upper subsoil (30 cm depth). The cores were drained to a range of matric potentials (ψ), and air permeability measured at ψ = -30 and ψ = -100 hPa. At all three locations, incorporation of straw increased SOC by ∼ 13% and ∼ 15% relative to removal and burning, respectively. Leaving straw in the field (chopped or burned) increased exchangeable potassium found in the soil layer 0–80 cm depth with approximately 110–400 kg per hectare, highest for the most clay-holding soil. Addition of straw decreased soil dry bulk density and increased the volume of soil pores holding water available for plants (0.2–30 µm), while no significant effect was found for pores>30 µm. For the two sandy loam soils, air permeability tended to be highest for soil with incorporation of straw. For one of the sandy loam soils, the effect was significant when normalized to unit volume of air-filled pore volume. No effects of straw management were found on the volume of soil pore fractions in the subsoil. However, the measurements of air permeability indicated more continuous pores for straw-amended soil in the generally dense plough pan layer. The long-term effects of straw may affect important soil functions and ecosystem services.

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