Soil nitrous oxide emissions from a typical semiarid temperate steppe in inner Mongolia: effects of mineral nitrogen fertilizer levels and forms

• Published in: Plant and soil Vol. 342; no. 1/2; pp. 345 - 357
• Main Authors: Peng, Qin, Qi, Yuchun, Dong, Yunshe, Xiao, Shengsheng, He, Yating
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer 01-05-2011; Springer Netherlands; Springer Nature B.V
• Subjects: Agronomy. Soil science and plant productions; Ammonium; Ammonium compounds; Ammonium nitrate; Ammonium paratungstate; Animal, plant and microbial ecology; Biological and medical sciences; Biomedical and Life Sciences; Climate; Climate change; Ecology; Ecosystems; Emissions; Emissions (Pollution); Fertilizer industry; Fertilizers; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; Generalities. Analysis and diagnosis methods; Global temperature changes; Grassland soils; Grasslands; Greenhouse gases; Intergovernmental Panel on Climate Change; Life Sciences; Mineral fertilizers; Nitrogen; Nitrogen fertilization; Nitrogen fertilizers; Nitrogen, phosphorus, potassium fertilizations; Nitrous oxide; Plant Physiology; Plant Sciences; Pollutant emissions; Regular Article; Soil microorganisms; Soil samples; Soil science; Soil Science & Conservation; Soil treatment; Soil water; Soil water content; Soil-plant relationships. Soil fertility. Fertilization. Amendments; Soils; Steppes; Terrestrial ecosystems; Thawing; Nei Monggol; Asia; China; Far east; China, People's Rep., Inner Mongolia; N level; Grassland; Emission factor; Nitrous oxide; N form; Nitrogen oxide; Macronutrient(mineral); Typicality; Gas emission; Arid environment; Nitrogen compounds; Inorganic fertilizer; Inorganic element; Climatic zone; Temperate zone; Soils; Inorganic nitrogen; Steppe; Semi arid zone; N levels; Level; Nitrogen protoxide; Soil plant relation; Nitrogen fertilizer; Form factor
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1007/s11104-010-0699-1

Nitrous oxide (N2O) emissions can be significantly affected by the amounts and forms of nitrogen (N) available in soils, but the effect is highly dependent on local climate and soil conditions in specific ecosystem. To improve our understanding of the response of N2O emissions to different N sources of fertilizer in a typical semiarid temperate steppe in Inner Mongolia, a 2-year field experiment was conducted to investigate the effects of high, medium and low N fertilizer levels (HN: 200 kg Nha-1y-1, MN: 100 kg N ha-1y-1, and LN: 50 kg N ha-1y-1) respectively and N fertilizer forms (CAN: calcium ammonium nitrate, AS: ammonium sulphate and NS: sodium nitrate) on N2O emissions using static closed chamber method. Our data showed that peak N2O fluxes induced by N treatments were concentrated in short periods (2 to 3 weeks) after fertilization in summer and in soil thawing periods in early spring; there were similarly low N2O fluxes from all treatments in the remaining seasons of the year. The three N levels increased annual N2O emissions significantly (P<0.05) in the order of MN > HN > LN compared with the CK (control) treatment in year 1; in year 2, the elevation of annual N2O emissions was significant (P<0.05) by HN and MN treatments but was insignificant by LN treatments (P>0.05). The three N forms also had strong effects on N2O emissions. Significantly (P<0.05) higher annual N2O emissions were observed in the soils of CAN and AS fertilizer treatments than in the soils of NS fertilizer treatments in both measured years, but the difference between CAN and AS was not significant (P>0.05). Annual N2O emission factors (EF) ranged from 0.060 to 0.298% for different N fertilizer treatments in the two observed years, with an overall EF value of 0.125%. The EF values were by far less than the mean default EF proposed by the Intergovernmental Panel on Climate Change (IPCC).