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
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
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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).
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
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  surname: Peng
  fullname: Peng, Qin
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  givenname: Yuchun
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  givenname: Yunshe
  surname: Dong
  fullname: Dong, Yunshe
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  givenname: Shengsheng
  surname: Xiao
  fullname: Xiao, Shengsheng
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  givenname: Yating
  surname: He
  fullname: He, Yating
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ID FETCH-LOGICAL-c499t-ea485e2c6f405e465d8434a70e63234e30f45ea1436bc8c767b87b0c252fc8543
IEDL.DBID AEJHL
ISSN 0032-079X
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
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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
LinkModel DirectLink
MergedId FETCHMERGED-LOGICAL-c499t-ea485e2c6f405e465d8434a70e63234e30f45ea1436bc8c767b87b0c252fc8543
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SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
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PQPubID 23462
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proquest_journals_862190216
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crossref_primary_10_1007_s11104_010_0699_1
pascalfrancis_primary_24294919
springer_journals_10_1007_s11104_010_0699_1
jstor_primary_24130929
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
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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
URI https://www.jstor.org/stable/24130929
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