Methanotrophs are favored under hypoxia in ammonium-fertilized soils
Methanotrophy of arable soils is affected by N fertilization, but the knowledge about the effect of oxygen level is poorly understood; soil aeration can fluctuate and zones of low oxygen are widespread in soil. We monitored CH 4 oxidation in three mineral soils (Eutric Cambisol, Haplic Podzol, Molli...
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| Veröffentlicht in: | Biology and fertility of soils 2018-10, Vol.54 (7), p.861-870 |
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| creator | Walkiewicz, A. Brzezińska, M. Bieganowski, A. |
| description | Methanotrophy of arable soils is affected by N fertilization, but the knowledge about the effect of oxygen level is poorly understood; soil aeration can fluctuate and zones of low oxygen are widespread in soil. We monitored CH
4
oxidation in three mineral soils (Eutric Cambisol, Haplic Podzol, Mollic Gleysol) under laboratory conditions by varying the O
2
level (from 20 to 2% O
2
), with or without NH
4
+
(100 mg N kg
−1
). In controls (without NH
4
+
), CH
4
was oxidized completely in the O
2
range from oxia (20% O
2
) to high hypoxia (5% O
2
), while the process was inhibited under microoxia (2% O
2
). Ammonium application decreased CH
4
consumption in all soils. This negative effect was stronger at 20% and 2% O
2
than under hypoxia. The highest CH
4
oxidation rates and the shortest initial (lag) phases in both control and NH
4
+
-amended soils were observed under high (5% O
2
) and low (10% O
2
) hypoxia. |
| doi_str_mv | 10.1007/s00374-018-1302-9 |
| format | Article |
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4
oxidation in three mineral soils (Eutric Cambisol, Haplic Podzol, Mollic Gleysol) under laboratory conditions by varying the O
2
level (from 20 to 2% O
2
), with or without NH
4
+
(100 mg N kg
−1
). In controls (without NH
4
+
), CH
4
was oxidized completely in the O
2
range from oxia (20% O
2
) to high hypoxia (5% O
2
), while the process was inhibited under microoxia (2% O
2
). Ammonium application decreased CH
4
consumption in all soils. This negative effect was stronger at 20% and 2% O
2
than under hypoxia. The highest CH
4
oxidation rates and the shortest initial (lag) phases in both control and NH
4
+
-amended soils were observed under high (5% O
2
) and low (10% O
2
) hypoxia.</description><identifier>ISSN: 0178-2762</identifier><identifier>EISSN: 1432-0789</identifier><identifier>DOI: 10.1007/s00374-018-1302-9</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Aeration ; Agriculture ; Ammonium ; Ammonium compounds ; Arable land ; Biological fertilization ; Biomedical and Life Sciences ; Fertilization ; Hypoxia ; Life Sciences ; Methane ; Methanotrophic bacteria ; Original Article ; Oxidation ; Oxygen ; Podzolic soils ; Soil ; Soil aeration ; Soil amendment ; Soil Science & Conservation</subject><ispartof>Biology and fertility of soils, 2018-10, Vol.54 (7), p.861-870</ispartof><rights>The Author(s) 2018</rights><rights>Biology and Fertility of Soils is a copyright of Springer, (2018). All Rights Reserved. © 2018. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c359t-b6f62ec348dab78f40f8bed2f10eaf09f60a6c412ea31fdd76c03a4092bef6263</citedby><cites>FETCH-LOGICAL-c359t-b6f62ec348dab78f40f8bed2f10eaf09f60a6c412ea31fdd76c03a4092bef6263</cites><orcidid>0000-0003-4194-780X</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/s00374-018-1302-9$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00374-018-1302-9$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Walkiewicz, A.</creatorcontrib><creatorcontrib>Brzezińska, M.</creatorcontrib><creatorcontrib>Bieganowski, A.</creatorcontrib><title>Methanotrophs are favored under hypoxia in ammonium-fertilized soils</title><title>Biology and fertility of soils</title><addtitle>Biol Fertil Soils</addtitle><description>Methanotrophy of arable soils is affected by N fertilization, but the knowledge about the effect of oxygen level is poorly understood; soil aeration can fluctuate and zones of low oxygen are widespread in soil. We monitored CH
4
oxidation in three mineral soils (Eutric Cambisol, Haplic Podzol, Mollic Gleysol) under laboratory conditions by varying the O
2
level (from 20 to 2% O
2
), with or without NH
4
+
(100 mg N kg
−1
). In controls (without NH
4
+
), CH
4
was oxidized completely in the O
2
range from oxia (20% O
2
) to high hypoxia (5% O
2
), while the process was inhibited under microoxia (2% O
2
). Ammonium application decreased CH
4
consumption in all soils. This negative effect was stronger at 20% and 2% O
2
than under hypoxia. The highest CH
4
oxidation rates and the shortest initial (lag) phases in both control and NH
4
+
-amended soils were observed under high (5% O
2
) and low (10% O
2
) hypoxia.</description><subject>Aeration</subject><subject>Agriculture</subject><subject>Ammonium</subject><subject>Ammonium compounds</subject><subject>Arable land</subject><subject>Biological fertilization</subject><subject>Biomedical and Life Sciences</subject><subject>Fertilization</subject><subject>Hypoxia</subject><subject>Life Sciences</subject><subject>Methane</subject><subject>Methanotrophic bacteria</subject><subject>Original Article</subject><subject>Oxidation</subject><subject>Oxygen</subject><subject>Podzolic soils</subject><subject>Soil</subject><subject>Soil aeration</subject><subject>Soil amendment</subject><subject>Soil Science & Conservation</subject><issn>0178-2762</issn><issn>1432-0789</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>BENPR</sourceid><recordid>eNp1kDtPwzAURi0EEqXwA9giMRuuH_VjRAUKUhELzJaT2NRVEwc7QZRfT6ogMTHd5ZzvSgehSwLXBEDeZAAmOQaiMGFAsT5CM8IZxSCVPkYzIFJhKgU9RWc5bwHIQhE9Q3fPrt_YNvYpdptc2OQKbz9jcnUxtLVLxWbfxa9gi9AWtmliG4YGe5f6sAvfI5Rj2OVzdOLtLruL3ztHbw_3r8tHvH5ZPS1v17hiC93jUnhBXcW4qm0plefgVelq6gk460F7AVZUnFBnGfF1LUUFzHLQtHSjKdgcXU27XYofg8u92cYhteNLQ0ESDgsNeqTIRFUp5pycN10KjU17Q8AcYpkplhljmUMsc3Do5OSRbd9d-lv-X_oBLzxtcw</recordid><startdate>20181001</startdate><enddate>20181001</enddate><creator>Walkiewicz, A.</creator><creator>Brzezińska, M.</creator><creator>Bieganowski, A.</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7T7</scope><scope>7UA</scope><scope>7X2</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</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>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M0K</scope><scope>M2P</scope><scope>M7P</scope><scope>P64</scope><scope>PATMY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0003-4194-780X</orcidid></search><sort><creationdate>20181001</creationdate><title>Methanotrophs are favored under hypoxia in ammonium-fertilized soils</title><author>Walkiewicz, A. ; Brzezińska, M. ; Bieganowski, A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c359t-b6f62ec348dab78f40f8bed2f10eaf09f60a6c412ea31fdd76c03a4092bef6263</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Aeration</topic><topic>Agriculture</topic><topic>Ammonium</topic><topic>Ammonium compounds</topic><topic>Arable land</topic><topic>Biological fertilization</topic><topic>Biomedical and Life Sciences</topic><topic>Fertilization</topic><topic>Hypoxia</topic><topic>Life Sciences</topic><topic>Methane</topic><topic>Methanotrophic bacteria</topic><topic>Original Article</topic><topic>Oxidation</topic><topic>Oxygen</topic><topic>Podzolic soils</topic><topic>Soil</topic><topic>Soil aeration</topic><topic>Soil amendment</topic><topic>Soil Science & Conservation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Walkiewicz, A.</creatorcontrib><creatorcontrib>Brzezińska, M.</creatorcontrib><creatorcontrib>Bieganowski, A.</creatorcontrib><collection>Springer Nature OA/Free Journals</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Water Resources Abstracts</collection><collection>Agricultural Science Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science 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 One Sustainability</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>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Environmental Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Biology and fertility of soils</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Walkiewicz, A.</au><au>Brzezińska, M.</au><au>Bieganowski, A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Methanotrophs are favored under hypoxia in ammonium-fertilized soils</atitle><jtitle>Biology and fertility of soils</jtitle><stitle>Biol Fertil Soils</stitle><date>2018-10-01</date><risdate>2018</risdate><volume>54</volume><issue>7</issue><spage>861</spage><epage>870</epage><pages>861-870</pages><issn>0178-2762</issn><eissn>1432-0789</eissn><abstract>Methanotrophy of arable soils is affected by N fertilization, but the knowledge about the effect of oxygen level is poorly understood; soil aeration can fluctuate and zones of low oxygen are widespread in soil. We monitored CH
4
oxidation in three mineral soils (Eutric Cambisol, Haplic Podzol, Mollic Gleysol) under laboratory conditions by varying the O
2
level (from 20 to 2% O
2
), with or without NH
4
+
(100 mg N kg
−1
). In controls (without NH
4
+
), CH
4
was oxidized completely in the O
2
range from oxia (20% O
2
) to high hypoxia (5% O
2
), while the process was inhibited under microoxia (2% O
2
). Ammonium application decreased CH
4
consumption in all soils. This negative effect was stronger at 20% and 2% O
2
than under hypoxia. The highest CH
4
oxidation rates and the shortest initial (lag) phases in both control and NH
4
+
-amended soils were observed under high (5% O
2
) and low (10% O
2
) hypoxia.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00374-018-1302-9</doi><tpages>10</tpages><orcidid>https://orcid.org/0000-0003-4194-780X</orcidid><oa>free_for_read</oa></addata></record> |
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| language | eng |
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| source | SpringerLink Journals - AutoHoldings |
| subjects | Aeration Agriculture Ammonium Ammonium compounds Arable land Biological fertilization Biomedical and Life Sciences Fertilization Hypoxia Life Sciences Methane Methanotrophic bacteria Original Article Oxidation Oxygen Podzolic soils Soil Soil aeration Soil amendment Soil Science & Conservation |
| title | Methanotrophs are favored under hypoxia in ammonium-fertilized soils |
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