Soil nitrous oxide emissions from a typical semiarid temperate steppe in inner Mongolia: effects of mineral nitrogen fertilizer levels and forms
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...
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Published in: | Plant and soil Vol. 342; no. 1/2; pp. 345 - 357 |
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Language: | English |
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01-05-2011
Springer Netherlands Springer Nature B.V |
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Abstract | 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). |
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AbstractList | 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). Nitrous oxide ([N.sub.2]O) 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 [N.sub.2]O 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 N[ha.sup.-1][y.sup.-1], MN: 100 kg N [ha.sup.-1][y.sup.-1], and LN: 50 kg N [ha.sup.-1][y.sup.-1]) respectively and N fertilizer forms (CAN: calcium ammonium nitrate, AS: ammonium sulphate and NS: sodium nitrate) on [N.sub.2]O emissions using static closed chamber method. Our data showed that peak [N.sub.2]O 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 [N.sub.2]O fluxes from all treatments in the remaining seasons of the year. The three N levels increased annual [N.sub.2]O 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 [N.sub.2]O 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 [N.sub.2]O emissions. Significantly (P < 0.05) higher annual [N.sub.2]O 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 [N.sub.2]O 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). Keywords Nitrous oxide * N level * N form * Emission factor * Grassland 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^sup -1^y^sup -1^, MN: 100 kg N ha^sup -1^y^sup -1^, and LN: 50 kg N ha^sup -1^y^sup -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).[PUBLICATION ABSTRACT] Nitrous oxide ([N.sub.2]O) 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 [N.sub.2]O 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 N[ha.sup.-1][y.sup.-1], MN: 100 kg N [ha.sup.-1][y.sup.-1], and LN: 50 kg N [ha.sup.-1][y.sup.-1]) respectively and N fertilizer forms (CAN: calcium ammonium nitrate, AS: ammonium sulphate and NS: sodium nitrate) on [N.sub.2]O emissions using static closed chamber method. Our data showed that peak [N.sub.2]O 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 [N.sub.2]O fluxes from all treatments in the remaining seasons of the year. The three N levels increased annual [N.sub.2]O 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 [N.sub.2]O 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 [N.sub.2]O emissions. Significantly (P < 0.05) higher annual [N.sub.2]O 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 [N.sub.2]O 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). Nitrous oxide (N sub(2)O) 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 N sub(2)O 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 super(-1)y super( -1), MN: 100 kg N ha super(-1)y super(-1), and LN: 50 kg N ha super(-1)y super(-1)) respectively and N fertilizer forms (CAN: calcium ammonium nitrate, AS: ammonium sulphate and NS: sodium nitrate) on N sub(2)O emissions using static closed chamber method. Our data showed that peak N sub(2)O 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 N sub(2)O fluxes from all treatments in the remaining seasons of the year. The three N levels increased annual N sub(2)O 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 N sub(2)O 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 N sub(2)O emissions. Significantly (P<0.05) higher annual N sub(2)O 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 N sub(2)O 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). Nitrous oxide (N 2 O) 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 N 2 O 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 N ha -1 y -1 , MN: 100 kg N ha -1 y -1 , and LN: 50 kg N ha -1 y -1 ) respectively and N fertilizer forms (CAN: calcium ammonium nitrate, AS: ammonium sulphate and NS: sodium nitrate) on N 2 O emissions using static closed chamber method. Our data showed that peak N 2 O 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 N 2 O fluxes from all treatments in the remaining seasons of the year. The three N levels increased annual N 2 O 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 N 2 O 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 N 2 O emissions. Significantly ( P < 0.05) higher annual N 2 O 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 N 2 O 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). |
Audience | Academic |
Author | He, Yating Peng, Qin Dong, Yunshe Qi, Yuchun Xiao, Shengsheng |
Author_xml | – sequence: 1 givenname: Qin surname: Peng fullname: Peng, Qin – sequence: 2 givenname: Yuchun surname: Qi fullname: Qi, Yuchun – sequence: 3 givenname: Yunshe surname: Dong fullname: Dong, Yunshe – sequence: 4 givenname: Shengsheng surname: Xiao fullname: Xiao, Shengsheng – sequence: 5 givenname: Yating surname: He fullname: He, Yating |
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IngestDate | Tue Aug 27 04:46:41 EDT 2024 Fri Oct 25 11:15:10 EDT 2024 Fri Nov 08 04:26:12 EST 2024 Tue Nov 19 20:58:08 EST 2024 Tue Nov 12 22:55:38 EST 2024 Thu Nov 21 21:20:54 EST 2024 Sun Oct 22 16:07:18 EDT 2023 Sat Dec 16 12:02:13 EST 2023 Mon Nov 25 04:42:35 EST 2024 |
IsPeerReviewed | true |
IsScholarly | true |
Issue | 1/2 |
Keywords | 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 |
Language | English |
License | CC BY 4.0 |
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PublicationCentury | 2000 |
PublicationDate | 2011-05-01 |
PublicationDateYYYYMMDD | 2011-05-01 |
PublicationDate_xml | – month: 05 year: 2011 text: 2011-05-01 day: 01 |
PublicationDecade | 2010 |
PublicationPlace | Dordrecht |
PublicationPlace_xml | – name: Dordrecht |
PublicationSubtitle | An International Journal on Plant-Soil Relationships |
PublicationTitle | Plant and soil |
PublicationTitleAbbrev | Plant Soil |
PublicationYear | 2011 |
Publisher | Springer Springer Netherlands Springer Nature B.V |
Publisher_xml | – name: Springer – name: Springer Netherlands – name: Springer Nature B.V |
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Snippet | 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... Nitrous oxide (N 2 O) emissions can be significantly affected by the amounts and forms of nitrogen (N) available in soils, but the effect is highly dependent... Nitrous oxide ([N.sub.2]O) emissions can be significantly affected by the amounts and forms of nitrogen (N) available in soils, but the effect is highly... Nitrous oxide (N sub(2)O) emissions can be significantly affected by the amounts and forms of nitrogen (N) available in soils, but the effect is highly... |
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SubjectTerms | 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 |
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Title | Soil nitrous oxide emissions from a typical semiarid temperate steppe in inner Mongolia: effects of mineral nitrogen fertilizer levels and forms |
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