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Soil organic carbon patterns and carbon‑iron binding at different slope positions on eroded slopes in subalpine regions
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DOI:10.1016/j.catena.2026.110483.png)
Abstract
En 中文
• The middle slope of the subalpine road cut-slope is the area with the most severe erosion-induced carbon loss. • Mineral protection is still an important way of OC sequestration on alpine erode slopes. • Increased 2–0.25 mm aggregates content is significantly correlated with reduced Fe-OC on eroded slopes. • POC, Fe-OC and Fep are important indicators to predict soil erosion. • Hydrolytic enzymes and oxidases accelerate turnover of POC and Fe-OC at a higher degree of erosion.
Keywords:
Slope positions
Soil organic carbon patterns
Carbon‑iron binding
Iron oxides
Soil erosion
Subalpine regions
Journal
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