Nitrous oxide emissions from red clover and winter wheat residues depend on interacting effects of distribution, soil N availability and moisture level
Aim The effects of residue type and distribution, soil moisture and NO 3 − availability were investigated in 43 days laboratory incubations (15 °C) on emissions of N 2 O, CO 2 , and for some treatments NO and NH 3 . Methods Two crop residues were considered (red clover, RC, and winter wheat, WW), an...
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| Veröffentlicht in: | Plant and soil 2021-09, Vol.466 (1-2), p.121-138 |
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| creator | Taghizadeh-Toosi, Arezoo Janz, Baldur Labouriau, Rodrigo Olesen, Jørgen E. Butterbach-Bahl, Klaus Petersen, Søren O. |
| description | Aim
The effects of residue type and distribution, soil moisture and NO
3
−
availability were investigated in 43 days laboratory incubations (15 °C) on emissions of N
2
O, CO
2
, and for some treatments NO and NH
3
.
Methods
Two crop residues were considered (red clover, RC, and winter wheat, WW), and they were either mixed with topsoil, placed as a discrete layer in soil, or no addition. Soil NO
3
−
was either at ambient level or increased. Water filled pore space (WFPS) was adjusted to either 40 or 60%. All treatments were analysed for mineral N, N
2
O and CO
2
with manual sampling and gas chromatography. Selected treatments were analysed with a continuous-flow method of N
2
O and CO
2
by laser spectroscopy, NO by photoluminescence and NH
3
by acid traps.
Results
The NH
3
and NO emissions was higher in mixed RC than control and WW treatment. The N
2
O emission was many-fold higher with mixed than layered distribution, but only with high soil NO
3
−
availability and high soil moisture. Emissions of N
2
O from WW were an order of magnitude lower compared to RC, and decomposition was slower. Both batch and continuous-flow incubations resulted in similar emissions. Disregarding the extreme emissions in the high WFPS and NO
3
−
treatment, the N
2
O emission factors averaged 0.3 and 0.6% of residue N for WW and RC, respectively.
Conclusion
Residue decomposition was enhanced by mixing, and N
2
O emissions by higher soil water and NO
3
−
content. The results show the importance of residue distribution and soil condition on estimating N
2
O emission factors for crops. |
| doi_str_mv | 10.1007/s11104-021-05030-8 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_journals_2572354724</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A675517193</galeid><sourcerecordid>A675517193</sourcerecordid><originalsourceid>FETCH-LOGICAL-c386t-e728cd6fe191e676e5f427a50e66c148432760c933cc466336e94fc9c01bcb933</originalsourceid><addsrcrecordid>eNp9UctOHDEQtKIgZYH8QE6WcmWIHzP2zBGhEJAQXEDiZnk97Y3RrL3YngW-JL-bZjcSihRFPtjdXVXt7iLkC2ennDH9rXDOWdswwRvWMcma_gNZ8E7LBiP1kSwYk6Jhenj4RA5LeWRvMVcL8usm1JzmQtNLGIHCOpQSUizU57SmGUbqprSFTG0c6XOIFZ_PP8FWrJUwzlDoCBvAYop0V7auhrii4D24irqejqHUHJZzReETWlKY6A21WxsmuwxTqK878XVC2JyBTrCF6ZgceDsV-PznPiL3F9_vzi-b69sfV-dn142TvaoNaNG7UXngAwelFXS-Fdp2DJRyvO1bKbRibpDSuVYpKRUMrXeDY3zplpg-Il_3upucnnCaah7TnCO2NKLTQnatFu07amUnMCH6VHFO3JUzZ0p3Hdd8p3X6DxSeEdfqUgQfMP8XQewJLqdSMnizyWFt86vhzLz5ava-GvTV7Hw1PZLknlQQHFeQ33_8H9Zv08am0Q</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2572354724</pqid></control><display><type>article</type><title>Nitrous oxide emissions from red clover and winter wheat residues depend on interacting effects of distribution, soil N availability and moisture level</title><source>SpringerLink Journals</source><creator>Taghizadeh-Toosi, Arezoo ; Janz, Baldur ; Labouriau, Rodrigo ; Olesen, Jørgen E. ; Butterbach-Bahl, Klaus ; Petersen, Søren O.</creator><creatorcontrib>Taghizadeh-Toosi, Arezoo ; Janz, Baldur ; Labouriau, Rodrigo ; Olesen, Jørgen E. ; Butterbach-Bahl, Klaus ; Petersen, Søren O.</creatorcontrib><description>Aim
The effects of residue type and distribution, soil moisture and NO
3
−
availability were investigated in 43 days laboratory incubations (15 °C) on emissions of N
2
O, CO
2
, and for some treatments NO and NH
3
.
Methods
Two crop residues were considered (red clover, RC, and winter wheat, WW), and they were either mixed with topsoil, placed as a discrete layer in soil, or no addition. Soil NO
3
−
was either at ambient level or increased. Water filled pore space (WFPS) was adjusted to either 40 or 60%. All treatments were analysed for mineral N, N
2
O and CO
2
with manual sampling and gas chromatography. Selected treatments were analysed with a continuous-flow method of N
2
O and CO
2
by laser spectroscopy, NO by photoluminescence and NH
3
by acid traps.
Results
The NH
3
and NO emissions was higher in mixed RC than control and WW treatment. The N
2
O emission was many-fold higher with mixed than layered distribution, but only with high soil NO
3
−
availability and high soil moisture. Emissions of N
2
O from WW were an order of magnitude lower compared to RC, and decomposition was slower. Both batch and continuous-flow incubations resulted in similar emissions. Disregarding the extreme emissions in the high WFPS and NO
3
−
treatment, the N
2
O emission factors averaged 0.3 and 0.6% of residue N for WW and RC, respectively.
Conclusion
Residue decomposition was enhanced by mixing, and N
2
O emissions by higher soil water and NO
3
−
content. The results show the importance of residue distribution and soil condition on estimating N
2
O emission factors for crops.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-021-05030-8</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Agriculture ; Ammonia ; Analysis ; Availability ; Biomedical and Life Sciences ; Carbon dioxide ; Continuous flow ; Crop residues ; Decomposition ; Ecology ; Emissions ; Gas chromatography ; Identification and classification ; Life Sciences ; Moisture content ; Nitrogen content ; Nitrous oxide ; Photoluminescence ; Photons ; Physiological aspects ; Plant Physiology ; Plant Sciences ; Red clover ; Regular Article ; Residues ; Soil conditions ; Soil investigations ; Soil layers ; Soil moisture ; Soil Science & Conservation ; Soil water ; Soils ; Spectroscopy ; Topsoil ; Trifolium pratense ; Triticum aestivum ; Wheat ; Winter wheat</subject><ispartof>Plant and soil, 2021-09, Vol.466 (1-2), p.121-138</ispartof><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2021</rights><rights>COPYRIGHT 2021 Springer</rights><rights>The Author(s), under exclusive licence to Springer Nature Switzerland AG 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c386t-e728cd6fe191e676e5f427a50e66c148432760c933cc466336e94fc9c01bcb933</citedby><cites>FETCH-LOGICAL-c386t-e728cd6fe191e676e5f427a50e66c148432760c933cc466336e94fc9c01bcb933</cites><orcidid>0000-0002-1525-1940</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11104-021-05030-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11104-021-05030-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Taghizadeh-Toosi, Arezoo</creatorcontrib><creatorcontrib>Janz, Baldur</creatorcontrib><creatorcontrib>Labouriau, Rodrigo</creatorcontrib><creatorcontrib>Olesen, Jørgen E.</creatorcontrib><creatorcontrib>Butterbach-Bahl, Klaus</creatorcontrib><creatorcontrib>Petersen, Søren O.</creatorcontrib><title>Nitrous oxide emissions from red clover and winter wheat residues depend on interacting effects of distribution, soil N availability and moisture level</title><title>Plant and soil</title><addtitle>Plant Soil</addtitle><description>Aim
The effects of residue type and distribution, soil moisture and NO
3
−
availability were investigated in 43 days laboratory incubations (15 °C) on emissions of N
2
O, CO
2
, and for some treatments NO and NH
3
.
Methods
Two crop residues were considered (red clover, RC, and winter wheat, WW), and they were either mixed with topsoil, placed as a discrete layer in soil, or no addition. Soil NO
3
−
was either at ambient level or increased. Water filled pore space (WFPS) was adjusted to either 40 or 60%. All treatments were analysed for mineral N, N
2
O and CO
2
with manual sampling and gas chromatography. Selected treatments were analysed with a continuous-flow method of N
2
O and CO
2
by laser spectroscopy, NO by photoluminescence and NH
3
by acid traps.
Results
The NH
3
and NO emissions was higher in mixed RC than control and WW treatment. The N
2
O emission was many-fold higher with mixed than layered distribution, but only with high soil NO
3
−
availability and high soil moisture. Emissions of N
2
O from WW were an order of magnitude lower compared to RC, and decomposition was slower. Both batch and continuous-flow incubations resulted in similar emissions. Disregarding the extreme emissions in the high WFPS and NO
3
−
treatment, the N
2
O emission factors averaged 0.3 and 0.6% of residue N for WW and RC, respectively.
Conclusion
Residue decomposition was enhanced by mixing, and N
2
O emissions by higher soil water and NO
3
−
content. The results show the importance of residue distribution and soil condition on estimating N
2
O emission factors for crops.</description><subject>Agriculture</subject><subject>Ammonia</subject><subject>Analysis</subject><subject>Availability</subject><subject>Biomedical and Life Sciences</subject><subject>Carbon dioxide</subject><subject>Continuous flow</subject><subject>Crop residues</subject><subject>Decomposition</subject><subject>Ecology</subject><subject>Emissions</subject><subject>Gas chromatography</subject><subject>Identification and classification</subject><subject>Life Sciences</subject><subject>Moisture content</subject><subject>Nitrogen content</subject><subject>Nitrous oxide</subject><subject>Photoluminescence</subject><subject>Photons</subject><subject>Physiological aspects</subject><subject>Plant Physiology</subject><subject>Plant Sciences</subject><subject>Red clover</subject><subject>Regular Article</subject><subject>Residues</subject><subject>Soil conditions</subject><subject>Soil investigations</subject><subject>Soil layers</subject><subject>Soil moisture</subject><subject>Soil Science & Conservation</subject><subject>Soil water</subject><subject>Soils</subject><subject>Spectroscopy</subject><subject>Topsoil</subject><subject>Trifolium pratense</subject><subject>Triticum aestivum</subject><subject>Wheat</subject><subject>Winter wheat</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9UctOHDEQtKIgZYH8QE6WcmWIHzP2zBGhEJAQXEDiZnk97Y3RrL3YngW-JL-bZjcSihRFPtjdXVXt7iLkC2ennDH9rXDOWdswwRvWMcma_gNZ8E7LBiP1kSwYk6Jhenj4RA5LeWRvMVcL8usm1JzmQtNLGIHCOpQSUizU57SmGUbqprSFTG0c6XOIFZ_PP8FWrJUwzlDoCBvAYop0V7auhrii4D24irqejqHUHJZzReETWlKY6A21WxsmuwxTqK878XVC2JyBTrCF6ZgceDsV-PznPiL3F9_vzi-b69sfV-dn142TvaoNaNG7UXngAwelFXS-Fdp2DJRyvO1bKbRibpDSuVYpKRUMrXeDY3zplpg-Il_3upucnnCaah7TnCO2NKLTQnatFu07amUnMCH6VHFO3JUzZ0p3Hdd8p3X6DxSeEdfqUgQfMP8XQewJLqdSMnizyWFt86vhzLz5ava-GvTV7Hw1PZLknlQQHFeQ33_8H9Zv08am0Q</recordid><startdate>20210901</startdate><enddate>20210901</enddate><creator>Taghizadeh-Toosi, Arezoo</creator><creator>Janz, Baldur</creator><creator>Labouriau, Rodrigo</creator><creator>Olesen, Jørgen E.</creator><creator>Butterbach-Bahl, Klaus</creator><creator>Petersen, Søren O.</creator><general>Springer International Publishing</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>88A</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>P64</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-1525-1940</orcidid></search><sort><creationdate>20210901</creationdate><title>Nitrous oxide emissions from red clover and winter wheat residues depend on interacting effects of distribution, soil N availability and moisture level</title><author>Taghizadeh-Toosi, Arezoo ; Janz, Baldur ; Labouriau, Rodrigo ; Olesen, Jørgen E. ; Butterbach-Bahl, Klaus ; Petersen, Søren O.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c386t-e728cd6fe191e676e5f427a50e66c148432760c933cc466336e94fc9c01bcb933</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Agriculture</topic><topic>Ammonia</topic><topic>Analysis</topic><topic>Availability</topic><topic>Biomedical and Life Sciences</topic><topic>Carbon dioxide</topic><topic>Continuous flow</topic><topic>Crop residues</topic><topic>Decomposition</topic><topic>Ecology</topic><topic>Emissions</topic><topic>Gas chromatography</topic><topic>Identification and classification</topic><topic>Life Sciences</topic><topic>Moisture content</topic><topic>Nitrogen content</topic><topic>Nitrous oxide</topic><topic>Photoluminescence</topic><topic>Photons</topic><topic>Physiological aspects</topic><topic>Plant Physiology</topic><topic>Plant Sciences</topic><topic>Red clover</topic><topic>Regular Article</topic><topic>Residues</topic><topic>Soil conditions</topic><topic>Soil investigations</topic><topic>Soil layers</topic><topic>Soil moisture</topic><topic>Soil Science & Conservation</topic><topic>Soil water</topic><topic>Soils</topic><topic>Spectroscopy</topic><topic>Topsoil</topic><topic>Trifolium pratense</topic><topic>Triticum aestivum</topic><topic>Wheat</topic><topic>Winter wheat</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Taghizadeh-Toosi, Arezoo</creatorcontrib><creatorcontrib>Janz, Baldur</creatorcontrib><creatorcontrib>Labouriau, Rodrigo</creatorcontrib><creatorcontrib>Olesen, Jørgen E.</creatorcontrib><creatorcontrib>Butterbach-Bahl, Klaus</creatorcontrib><creatorcontrib>Petersen, Søren O.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Taghizadeh-Toosi, Arezoo</au><au>Janz, Baldur</au><au>Labouriau, Rodrigo</au><au>Olesen, Jørgen E.</au><au>Butterbach-Bahl, Klaus</au><au>Petersen, Søren O.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Nitrous oxide emissions from red clover and winter wheat residues depend on interacting effects of distribution, soil N availability and moisture level</atitle><jtitle>Plant and soil</jtitle><stitle>Plant Soil</stitle><date>2021-09-01</date><risdate>2021</risdate><volume>466</volume><issue>1-2</issue><spage>121</spage><epage>138</epage><pages>121-138</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><abstract>Aim
The effects of residue type and distribution, soil moisture and NO
3
−
availability were investigated in 43 days laboratory incubations (15 °C) on emissions of N
2
O, CO
2
, and for some treatments NO and NH
3
.
Methods
Two crop residues were considered (red clover, RC, and winter wheat, WW), and they were either mixed with topsoil, placed as a discrete layer in soil, or no addition. Soil NO
3
−
was either at ambient level or increased. Water filled pore space (WFPS) was adjusted to either 40 or 60%. All treatments were analysed for mineral N, N
2
O and CO
2
with manual sampling and gas chromatography. Selected treatments were analysed with a continuous-flow method of N
2
O and CO
2
by laser spectroscopy, NO by photoluminescence and NH
3
by acid traps.
Results
The NH
3
and NO emissions was higher in mixed RC than control and WW treatment. The N
2
O emission was many-fold higher with mixed than layered distribution, but only with high soil NO
3
−
availability and high soil moisture. Emissions of N
2
O from WW were an order of magnitude lower compared to RC, and decomposition was slower. Both batch and continuous-flow incubations resulted in similar emissions. Disregarding the extreme emissions in the high WFPS and NO
3
−
treatment, the N
2
O emission factors averaged 0.3 and 0.6% of residue N for WW and RC, respectively.
Conclusion
Residue decomposition was enhanced by mixing, and N
2
O emissions by higher soil water and NO
3
−
content. The results show the importance of residue distribution and soil condition on estimating N
2
O emission factors for crops.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s11104-021-05030-8</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0002-1525-1940</orcidid></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0032-079X |
| ispartof | Plant and soil, 2021-09, Vol.466 (1-2), p.121-138 |
| issn | 0032-079X 1573-5036 |
| language | eng |
| recordid | cdi_proquest_journals_2572354724 |
| source | SpringerLink Journals |
| subjects | Agriculture Ammonia Analysis Availability Biomedical and Life Sciences Carbon dioxide Continuous flow Crop residues Decomposition Ecology Emissions Gas chromatography Identification and classification Life Sciences Moisture content Nitrogen content Nitrous oxide Photoluminescence Photons Physiological aspects Plant Physiology Plant Sciences Red clover Regular Article Residues Soil conditions Soil investigations Soil layers Soil moisture Soil Science & Conservation Soil water Soils Spectroscopy Topsoil Trifolium pratense Triticum aestivum Wheat Winter wheat |
| title | Nitrous oxide emissions from red clover and winter wheat residues depend on interacting effects of distribution, soil N availability and moisture level |
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