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Long-term nitrous oxide fluxes in annual and perennial agricultural and unmanaged ecosystems in the upper Midwest USA.

Identifieur interne : 001783 ( Main/Exploration ); précédent : 001782; suivant : 001784

Long-term nitrous oxide fluxes in annual and perennial agricultural and unmanaged ecosystems in the upper Midwest USA.

Auteurs : Ilya Gelfand [États-Unis] ; Iurii Shcherbak [États-Unis] ; Neville Millar [États-Unis] ; Alexandra N. Kravchenko [États-Unis] ; G Philip Robertson [États-Unis]

Source :

RBID : pubmed:27510313

Descripteurs français

English descriptors

Abstract

Differences in soil nitrous oxide (N2 O) fluxes among ecosystems are often difficult to evaluate and predict due to high spatial and temporal variabilities and few direct experimental comparisons. For 20 years, we measured N2 O fluxes in 11 ecosystems in southwest Michigan USA: four annual grain crops (corn-soybean-wheat rotations) managed with conventional, no-till, reduced input, or biologically based/organic inputs; three perennial crops (alfalfa, poplar, and conifers); and four unmanaged ecosystems of different successional age including mature forest. Average N2 O emissions were higher from annual grain and N-fixing cropping systems than from nonleguminous perennial cropping systems and were low across unmanaged ecosystems. Among annual cropping systems full-rotation fluxes were indistinguishable from one another but rotation phase mattered. For example, those systems with cover crops and reduced fertilizer N emitted more N2 O during the corn and soybean phases, but during the wheat phase fluxes were ~40% lower. Likewise, no-till did not differ from conventional tillage over the entire rotation but reduced emissions ~20% in the wheat phase and increased emissions 30-80% in the corn and soybean phases. Greenhouse gas intensity for the annual crops (flux per unit yield) was lowest for soybeans produced under conventional management, while for the 11 other crop × management combinations intensities were similar to one another. Among the fertilized systems, emissions ranged from 0.30 to 1.33 kg N2 O-N ha-1  yr-1 and were best predicted by IPCC Tier 1 and ΔEF emission factor approaches. Annual cumulative fluxes from perennial systems were best explained by soil NO3- pools (r2  = 0.72) but not so for annual crops, where management differences overrode simple correlations. Daily soil N2 O emissions were poorly predicted by any measured variables. Overall, long-term measurements reveal lower fluxes in nonlegume perennial vegetation and, for conservatively fertilized annual crops, the overriding influence of rotation phase on annual fluxes.

DOI: 10.1111/gcb.13426
PubMed: 27510313


Affiliations:


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<div type="abstract" xml:lang="en">Differences in soil nitrous oxide (N
<sub>2</sub>
O) fluxes among ecosystems are often difficult to evaluate and predict due to high spatial and temporal variabilities and few direct experimental comparisons. For 20 years, we measured N
<sub>2</sub>
O fluxes in 11 ecosystems in southwest Michigan USA: four annual grain crops (corn-soybean-wheat rotations) managed with conventional, no-till, reduced input, or biologically based/organic inputs; three perennial crops (alfalfa, poplar, and conifers); and four unmanaged ecosystems of different successional age including mature forest. Average N
<sub>2</sub>
O emissions were higher from annual grain and N-fixing cropping systems than from nonleguminous perennial cropping systems and were low across unmanaged ecosystems. Among annual cropping systems full-rotation fluxes were indistinguishable from one another but rotation phase mattered. For example, those systems with cover crops and reduced fertilizer N emitted more N
<sub>2</sub>
O during the corn and soybean phases, but during the wheat phase fluxes were ~40% lower. Likewise, no-till did not differ from conventional tillage over the entire rotation but reduced emissions ~20% in the wheat phase and increased emissions 30-80% in the corn and soybean phases. Greenhouse gas intensity for the annual crops (flux per unit yield) was lowest for soybeans produced under conventional management, while for the 11 other crop × management combinations intensities were similar to one another. Among the fertilized systems, emissions ranged from 0.30 to 1.33 kg N
<sub>2</sub>
O-N ha
<sup>-1</sup>
 yr
<sup>-1</sup>
and were best predicted by IPCC Tier 1 and ΔEF emission factor approaches. Annual cumulative fluxes from perennial systems were best explained by soil NO3- pools (r
<sup>2</sup>
 = 0.72) but not so for annual crops, where management differences overrode simple correlations. Daily soil N
<sub>2</sub>
O emissions were poorly predicted by any measured variables. Overall, long-term measurements reveal lower fluxes in nonlegume perennial vegetation and, for conservatively fertilized annual crops, the overriding influence of rotation phase on annual fluxes.</div>
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<AbstractText>Differences in soil nitrous oxide (N
<sub>2</sub>
O) fluxes among ecosystems are often difficult to evaluate and predict due to high spatial and temporal variabilities and few direct experimental comparisons. For 20 years, we measured N
<sub>2</sub>
O fluxes in 11 ecosystems in southwest Michigan USA: four annual grain crops (corn-soybean-wheat rotations) managed with conventional, no-till, reduced input, or biologically based/organic inputs; three perennial crops (alfalfa, poplar, and conifers); and four unmanaged ecosystems of different successional age including mature forest. Average N
<sub>2</sub>
O emissions were higher from annual grain and N-fixing cropping systems than from nonleguminous perennial cropping systems and were low across unmanaged ecosystems. Among annual cropping systems full-rotation fluxes were indistinguishable from one another but rotation phase mattered. For example, those systems with cover crops and reduced fertilizer N emitted more N
<sub>2</sub>
O during the corn and soybean phases, but during the wheat phase fluxes were ~40% lower. Likewise, no-till did not differ from conventional tillage over the entire rotation but reduced emissions ~20% in the wheat phase and increased emissions 30-80% in the corn and soybean phases. Greenhouse gas intensity for the annual crops (flux per unit yield) was lowest for soybeans produced under conventional management, while for the 11 other crop × management combinations intensities were similar to one another. Among the fertilized systems, emissions ranged from 0.30 to 1.33 kg N
<sub>2</sub>
O-N ha
<sup>-1</sup>
 yr
<sup>-1</sup>
and were best predicted by IPCC Tier 1 and ΔEF emission factor approaches. Annual cumulative fluxes from perennial systems were best explained by soil NO3- pools (r
<sup>2</sup>
 = 0.72) but not so for annual crops, where management differences overrode simple correlations. Daily soil N
<sub>2</sub>
O emissions were poorly predicted by any measured variables. Overall, long-term measurements reveal lower fluxes in nonlegume perennial vegetation and, for conservatively fertilized annual crops, the overriding influence of rotation phase on annual fluxes.</AbstractText>
<CopyrightInformation>© 2016 The Authors. Global Change Biology Published by John Wiley & Sons Ltd.</CopyrightInformation>
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<Month>08</Month>
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<Country>England</Country>
<MedlineTA>Glob Chang Biol</MedlineTA>
<NlmUniqueID>9888746</NlmUniqueID>
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<NameOfSubstance UI="D012987">Soil</NameOfSubstance>
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<RegistryNumber>K50XQU1029</RegistryNumber>
<NameOfSubstance UI="D009609">Nitrous Oxide</NameOfSubstance>
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<DescriptorName UI="D000383" MajorTopicYN="N">Agriculture</DescriptorName>
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<DescriptorName UI="D018556" MajorTopicYN="N">Crops, Agricultural</DescriptorName>
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<DescriptorName UI="D008824" MajorTopicYN="N">Michigan</DescriptorName>
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<DescriptorName UI="D012987" MajorTopicYN="N">Soil</DescriptorName>
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</MeshHeadingList>
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<Keyword MajorTopicYN="Y">corn</Keyword>
<Keyword MajorTopicYN="Y">cover crops</Keyword>
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<Keyword MajorTopicYN="Y">forest</Keyword>
<Keyword MajorTopicYN="Y">nitrogen fertilizer</Keyword>
<Keyword MajorTopicYN="Y">no-till</Keyword>
<Keyword MajorTopicYN="Y">rotation phase</Keyword>
<Keyword MajorTopicYN="Y">soybean</Keyword>
<Keyword MajorTopicYN="Y">succession</Keyword>
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<Year>2016</Year>
<Month>06</Month>
<Day>15</Day>
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<Year>2016</Year>
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<ArticleIdList>
<ArticleId IdType="pubmed">27510313</ArticleId>
<ArticleId IdType="doi">10.1111/gcb.13426</ArticleId>
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</pubmed>
<affiliations>
<list>
<country>
<li>États-Unis</li>
</country>
<region>
<li>Michigan</li>
</region>
<settlement>
<li>East Lansing</li>
</settlement>
<orgName>
<li>Université d'État du Michigan</li>
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<tree>
<country name="États-Unis">
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<name sortKey="Gelfand, Ilya" sort="Gelfand, Ilya" uniqKey="Gelfand I" first="Ilya" last="Gelfand">Ilya Gelfand</name>
</region>
<name sortKey="Gelfand, Ilya" sort="Gelfand, Ilya" uniqKey="Gelfand I" first="Ilya" last="Gelfand">Ilya Gelfand</name>
<name sortKey="Kravchenko, Alexandra N" sort="Kravchenko, Alexandra N" uniqKey="Kravchenko A" first="Alexandra N" last="Kravchenko">Alexandra N. Kravchenko</name>
<name sortKey="Millar, Neville" sort="Millar, Neville" uniqKey="Millar N" first="Neville" last="Millar">Neville Millar</name>
<name sortKey="Millar, Neville" sort="Millar, Neville" uniqKey="Millar N" first="Neville" last="Millar">Neville Millar</name>
<name sortKey="Robertson, G Philip" sort="Robertson, G Philip" uniqKey="Robertson G" first="G Philip" last="Robertson">G Philip Robertson</name>
<name sortKey="Robertson, G Philip" sort="Robertson, G Philip" uniqKey="Robertson G" first="G Philip" last="Robertson">G Philip Robertson</name>
<name sortKey="Robertson, G Philip" sort="Robertson, G Philip" uniqKey="Robertson G" first="G Philip" last="Robertson">G Philip Robertson</name>
<name sortKey="Shcherbak, Iurii" sort="Shcherbak, Iurii" uniqKey="Shcherbak I" first="Iurii" last="Shcherbak">Iurii Shcherbak</name>
<name sortKey="Shcherbak, Iurii" sort="Shcherbak, Iurii" uniqKey="Shcherbak I" first="Iurii" last="Shcherbak">Iurii Shcherbak</name>
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