Abstract
How long-term tillage drives nitrogen (N) function succession by degrading vadose zone preferential flow paths remains unclear. This study investigated croplands across multiple tillage chronosequences by integrating dye tracing, 15 N isotope tracing, and metagenomic techniques. The study shows that tillage-induced degradation of preferential flow structures homogenizes the vadose zone and reshapes N-cycling communities, shifting denitrifiers from nirK - to nirS -dominated assemblages. Consistent with this community turnover, gross nitrification rates in shallow preferential paths are 30.8% higher than in the adjacent matrix in short-term tillage, whereas in deep layers matrix denitrification and DNRA rates exceed those in preferential paths by 37.9 and 76.1%, and anammox appears only in the matrix at medium- and long-term tillage, indicating a concentration of reductive N processes in the matrix. Path analysis further shows that tillage-driven alterations in hydraulic properties (path coefficient = −0.91, p < 0.01), together with these community and process-rate shifts, redirect the dominant N pathway from hotspot-driven nitrification in preferential channels to matrix-driven reductive N loss, converting a nitrate-leaching-prone system into one with higher gaseous emission potential. This establishes a mechanistic link linking soil hydraulic degradation to N functional succession and supports targeted, stage-dependent farmland nitrogen management.
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Claims 0
Judged adjacent: soil study without a plant endpoint — claims were not extracted. This is a scope decision by the model, not a statement about the paper’s findings.