ArticleiScience2026
Conservation tillage dominates pore formation freeze thaw cycles alleviate compaction in northeast China black soil.
Article in iScience, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
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Abstract
Conservation tillage (CT) enhances soil structure, but its interaction with freeze-thaw cycles on micropores remains unclear. This field study compared CT and rotary tillage (RT) by using X-ray computer tomography to analyze soil pore characteristics and physical properties. CT promoted large pores (>500 μm) forming stable preferential flow paths, while RT mainly developed medium-sized pores (200-400 μm). Freeze-thaw cycles increased >300 μm porosity by 5%, particularly in the 20-40 cm layer, an effect influenced by bulk density and freezing duration. Soil pore parameters contributed 35% and 48% to soil nutrients in the 0-20 cm and 20-40 cm layers, respectively. Overall, tillage dominates soil porosity formation, and freeze-thaw cycles play a supplementary role in alleviating compaction. These findings provide practical guidelines for integrating CT with natural freeze-thaw processes to sustain black soil health in cold regions.
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