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The contributions of hydroxylamine and nitrite to NO and N2O production in alkaline and acidic vegetable soils

  • Soils, Sec 5 • Soil and Landscape Ecology • Research Article
  • Published:
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Abstract

Purpose

The contribution of hydroxylamine (NH2OH) and nitrite (NO2) to nitric oxide (NO) and nitrous oxide (N2O) production remains unclear in vegetable production soils.

Materials and methods

Soils collected from six typical greenhouse vegetable fields were incubated for 48 h following amendment with 1 mM NaNO2, 10 μM NH2OH, or 1 mM NaNO2 + 10 μM NH2OH. The importance of abiotic processes on the NO and N2O formation from the NH2OH and NO2 were studied by irradiating the soil samples with γ-irradiation.

Results and discussion

NO2 amendment significantly stimulated NO production, while the NH2OH-dependent NO production was minimal. NH2OH stimulated more abiotic N2O production in alkaline soils than in acidic soils (p < 0.05), while NO2 stimulated more biotic N2O production in acidic soils than in alkaline soils (p < 0.05). The NH2OH- and NO2-dependent sources produced biotic or abiotic N2O with site preference (SP) values of 27.4–36.5‰, which is similar to those from ammonia-oxidizing archaea (AOA) or ammonia-oxidizing bacteria (AOB) sources (25.1–34.2‰), indicating that abiotic N2O production were closely linked with biotic NH3 oxidation. The variability of NO2+NH2OH-induced N2O production can be explained by the soil organic carbon and iron concentrations, whereas NO2-induced NO production can be explained by the soil pH.

Conclusions

NO2 addition dominated NO production in all soils. Furthermore, NO2 addition increased biotic N2O production in acidic soils, while NH2OH addition increased abiotic N2O production in alkaline soils. The presence of NO2 could significantly stimulate the abiotic conversion of NH2OH to N2O in soils with low soil organic carbon and high iron concentrations. Thus, assessing the abundance of NH2OH and NO2 could provide crucial information for understanding NO and N2O production procedures in vegetable soils.

Highlights

• The chemical decomposition of NO2 dominated NO production in all soils.

• The NH2OH stimulated abiotic N2O production in alkaline soils.

• The NO2 stimulated biotic N2O production in acidic soils.

• The SP for abiotic NO2-/NH2OH-related N2O were in the same range as AOB/AOA sources.

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Acknowledgments

We sincerely appreciate the anonymous reviewers and editors for their critical and valuable comments to help improve this manuscript.

Funding

This work was jointly supported by the National Natural Science Foundation of China (41977078, 41425005), the Special Fund for Agro-Scientific Research in the Public Interest (201503106), and the Postgraduate Research & Practice Innovation Program of Jiangsu Province, China (KYCX18_0678).

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Correspondence to Zhengqin Xiong.

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Duan, P., Shen, H., Jiang, X. et al. The contributions of hydroxylamine and nitrite to NO and N2O production in alkaline and acidic vegetable soils. J Soils Sediments 20, 2903–2911 (2020). https://doi.org/10.1007/s11368-020-02645-9

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