4.7 Article

Potential Nitrogen Mineralization and Its Availability in Response to Long-Term Fertilization in a Chinese Fluvo-Aquic Soil

Journal

AGRONOMY-BASEL
Volume 12, Issue 6, Pages -

Publisher

MDPI
DOI: 10.3390/agronomy12061260

Keywords

aerobic incubation; manure application; mineralization rate; NH4+ fixation; nitrification rate; nitrogen mineralization potential

Funding

  1. National Science Foundation of China [42077098]
  2. Fundamental Research Funds for Central Non-profit Scientific Institution [Y2022XK26]

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The study aimed to explore the effect of long-term fertilization on soil organic nitrogen mineralization potential and its impact on plant nitrogen accessibility. The results showed that long-term fertilization can increase the nitrogen mineralization rate in soil, suggesting that fertilization is an effective strategy to enhance soil nitrogen availability.
The determination of organic nitrogen (N) mineralization is crucial for estimating N availability, quantifying exogenous inputs, and estimating associated environmental impacts. The objective of this study was to explore the effect of long-term various fertilization on soil organic N mineralization potential (NMP), which influences plant N accessibility. Treatments from a 26-year long-term field experiment with no fertilization (CK), chemical fertilizer N at 165 kg N ha(-1) and P at 82.5 kg P2O5 ha(-1) (NP), NP with K fertilizer at 165, 82.5, 82.5 kg ha(-1) N, P2O5 and K2O (NPK), NPK at 165, 82.5, 82.5 kg ha(-1) N, P2O5 and K2O with manure at 7857.14 kg ha(-1) (NPKM), and NPKM at 165, 82.5, 82.5 kg ha(-1) N, P2O5 and K2O with manure at 1.5x application rate (11,785.71 kg ha(-1)) (1.5NPKM) were examined for potentially mineralizable N by aerobic incubation at 35 degrees C for 30 weeks. Three pools (Pools I, II, and III) of mineralizable N were recognized. Pool I, the mineralization flush on rewetting in the first 2 weeks; Pool II, gross N mineralization between weeks 2 and 30; and Pool III, the potentially mineralizable N, predicted from the fitted curve, that did not mineralize during the incubation period. Soil microbial biomass carbon (SMBC) and N (SMBN) as well as fixed ammonium (NH4+) contents and relationship with N mineralization rate (k) were also studied. Long-term manure application yielded a significantly higher k (0.32 week(-1)) than other treatments (0.12-0.22 week(-1)) but not a significantly higher NMP. Nitrogen mineralization during the wheat and maize-growing seasons was predicted to be 8.7-26.3 (mg N kg(-1) soil) and 25.9-42.1 (mg N kg(-1) soil), respectively. Both labile mineralizable N pools (Pools I and II) followed the same patterns in the treatments: 1.5NPKM > NPKM > NPK > NP > CK, while the reverse was true for stable N (Pool III). The significant positive correlation between k with SMBC and SMBN (R-2 = 0.93, p = 0.008 and R-2 = 0.94, p = 0.006) suggested that the higher mineralization rate might be contributed by the higher soil microbial biomass in NPKM. The trends of fixed NH4+ and mineralized N were coupled. Long-term manure application significantly improved the N mineralization rate in soil. Manure application is an effective strategy to enhance soil microbial biomass and soil N availability and has the potential to reduce the dependence upon chemical N fertilization.

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