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Tillage reversal did not reverse N fertilization enhanced C storage in a Black Chernozem and a Gray Luvisol

•N fertilization and tillage reversal increased organic C more for soil with low C.•Macroaggregates were the most important fraction for C storage.•N fertilization and tillage reversal enhanced macroaggregate formation in topsoils.•Tillage reversal did not offset N fertilization-increased C storage...

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Published in:Geoderma 2020-07, Vol.370, p.114355, Article 114355
Main Authors: Sun, Lei, Feng, Yongsheng, Dyck, Miles F, Puurveen, Dick, Chang, Scott X.
Format: Article
Language:English
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Summary:•N fertilization and tillage reversal increased organic C more for soil with low C.•Macroaggregates were the most important fraction for C storage.•N fertilization and tillage reversal enhanced macroaggregate formation in topsoils.•Tillage reversal did not offset N fertilization-increased C storage in topsoils. Nitrogen (N) fertilization and reversing land management from long-term no tillage (NT) to conventional tillage (tillage reversal; TR) may markedly alter soil carbon (C) dynamics. We studied the impact of N fertilization, N applied at 100 kg ha−1 yr−1 (N100) vs. no N application (N0), and tillage reversal (NT vs. TR) on soil aggregation and aggregate-associated C in top- (0–10) and subsoils (50–60 cm) in a Black Chernozem and a Gray Luvisol. Our results showed that soil organic C content was greater in N100 (1.74 g C kg−1) than in N0 (1.29 g C kg−1), and in TR (1.71 g C kg−1) than in NT (1.32 g C kg−1) only in the topsoil of the Gray Luvisol. Nitrogen fertilization and tillage reversal improved topsoil, but not subsoil mean weight diameter or the amount of large macroaggregates (>2000 μm). Topsoil aggregate-associated C was only increased (P 
ISSN:0016-7061
1872-6259
DOI:10.1016/j.geoderma.2020.114355