Impact of heavy traffic on soil macroporosity of two silty forest soils: Initial effect and short-term recovery

Publication date: April 2014
Source:Geoderma, Volumes 217–218
Author(s): N. Bottinelli , V. Hallaire , N. Goutal , P. Bonnaud , J. Ranger
Processes and rate of macroporosity changes following heavy traffic in forest ecosystems are seldom studied. The aim of this study was to determine the ability of forest soils to regenerate their macroporosity naturally. The study was performed on 2 silty temperate-forest soils classified as sensitive to compaction located in north-eastern France. Macroporosity was measured in control and trafficked plots at 3 depths (0–7, 15–30 and 30–45cm) over 2–3years. Soil macroporosity characteristics (shape, size and orientation) were assessed on polished sections through 2D-image analysis and micromorphic observations. Immediately after heavy traffic, macroporosity decreased by 96 to 49% from 0 to 45cm in depth. Natural regeneration of macroporosity occurred in the upper 7cm of soil, while the soil below remained compacted. Small and medium macropores (0.05–0.8mm²) dominated by rounded and irregular pores regenerated completely. Large macropores (>0.8mm²) originally dominated by vughs, mammilated vughs and channels rarely regenerated and were gradually replaced by horizontally oriented planar pores. Our results suggest that initial stages of natural macroporosity recovery are likely due to plant-root penetration and physical processes (shrink–swell, freeze–thaw), whereas recovery due to fauna activities appears later.