Effect of mowing on N2O and CH4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia

To assess the impacts of mowing on N 2 O and CH 4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia, China, two regimes were investigated: unmown since 2005 (UM), and mown once every three years since 2009 (M3). On-site measurements were conducted continuously during a year-round...

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Veröffentlicht in:Frontiers of earth science 2015-09, Vol.9 (3), p.473-486
Hauptverfasser: Lu, Zedong, Du, Rui, Du, Pengrui, Li, Ziming, Liang, Zongmin, Wang, Yaling, Qin, Saisai, Zhong, Lei
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container_title Frontiers of earth science
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creator Lu, Zedong
Du, Rui
Du, Pengrui
Li, Ziming
Liang, Zongmin
Wang, Yaling
Qin, Saisai
Zhong, Lei
description To assess the impacts of mowing on N 2 O and CH 4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia, China, two regimes were investigated: unmown since 2005 (UM), and mown once every three years since 2009 (M3). On-site measurements were conducted continuously during a year-round period (August 2011 to August 2012). During the observation period, three diurnal cycles were also measured. In addition, a targeted laboratory experiment was conducted to make up for the few measurements in winter. A large pulse of N 2 O emissions related to freeze-thaw cycles was observed at M3 during the spring thaw. Results showed that the meadow-steppes played a role as a sink for CH 4 and a source for N 2 O. Significantly lower mean CH 4 uptake at UM (40.3 μg C·m −2 ·h −1 ) as compared to M3 (70.5 μg C ·m −2 ·h −1 ) ( p
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On-site measurements were conducted continuously during a year-round period (August 2011 to August 2012). During the observation period, three diurnal cycles were also measured. In addition, a targeted laboratory experiment was conducted to make up for the few measurements in winter. A large pulse of N 2 O emissions related to freeze-thaw cycles was observed at M3 during the spring thaw. Results showed that the meadow-steppes played a role as a sink for CH 4 and a source for N 2 O. Significantly lower mean CH 4 uptake at UM (40.3 μg C·m −2 ·h −1 ) as compared to M3 (70.5 μg C ·m −2 ·h −1 ) ( p &lt;0.01), and significantly higher mean N 2 O efflux at UM (6.3 μgN·m −2 ·h −1 ) as compared to M3 (4.3 μg N·m −2 ·h −1 ) ( p &lt;0.05) were found. The laboratory experiment results revealed that mowing changed the soil conditions that favor the activity of denitrifiers during thawing periods. The CH 4 and N 2 O fluxes were significantly correlated with soil temperature ( p &lt;0.05). Mowing affected CH 4 uptake and N 2 O emission mainly through its effect on vegetation types and some soil properties, such as soil inorganic N content, soil temperature, and soil moisture content, while soil inorganic N and moisture were not leading factors. Our results also suggested that mowing could mitigate the potential global warming in terms of CH 4 uptake and N 2 O emissions.</description><identifier>ISSN: 2095-0195</identifier><identifier>EISSN: 2095-0209</identifier><identifier>DOI: 10.1007/s11707-014-0486-z</identifier><language>eng</language><publisher>Beijing: Higher Education Press</publisher><subject>Climate change ; Earth and Environmental Science ; Earth Sciences ; Emissions ; Global warming ; Grasslands ; Meadows ; Methane ; Moisture content ; Nitrous oxide ; Research Article ; Soil moisture ; Soil properties ; Soil temperature ; Steppes ; Thawing ; Vegetation effects</subject><ispartof>Frontiers of earth science, 2015-09, Vol.9 (3), p.473-486</ispartof><rights>Higher Education Press and Springer-Verlag Berlin Heidelberg 2014</rights><rights>Higher Education Press and Springer-Verlag Berlin Heidelberg 2015</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c386t-ad9058072a36e4a764bdff07d7c6ce0efaddfbecad275cfddd40526488874d823</citedby><cites>FETCH-LOGICAL-c386t-ad9058072a36e4a764bdff07d7c6ce0efaddfbecad275cfddd40526488874d823</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11707-014-0486-z$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11707-014-0486-z$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Lu, Zedong</creatorcontrib><creatorcontrib>Du, Rui</creatorcontrib><creatorcontrib>Du, Pengrui</creatorcontrib><creatorcontrib>Li, Ziming</creatorcontrib><creatorcontrib>Liang, Zongmin</creatorcontrib><creatorcontrib>Wang, Yaling</creatorcontrib><creatorcontrib>Qin, Saisai</creatorcontrib><creatorcontrib>Zhong, Lei</creatorcontrib><title>Effect of mowing on N2O and CH4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia</title><title>Frontiers of earth science</title><addtitle>Front. Earth Sci</addtitle><description>To assess the impacts of mowing on N 2 O and CH 4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia, China, two regimes were investigated: unmown since 2005 (UM), and mown once every three years since 2009 (M3). On-site measurements were conducted continuously during a year-round period (August 2011 to August 2012). During the observation period, three diurnal cycles were also measured. In addition, a targeted laboratory experiment was conducted to make up for the few measurements in winter. A large pulse of N 2 O emissions related to freeze-thaw cycles was observed at M3 during the spring thaw. Results showed that the meadow-steppes played a role as a sink for CH 4 and a source for N 2 O. Significantly lower mean CH 4 uptake at UM (40.3 μg C·m −2 ·h −1 ) as compared to M3 (70.5 μg C ·m −2 ·h −1 ) ( p &lt;0.01), and significantly higher mean N 2 O efflux at UM (6.3 μgN·m −2 ·h −1 ) as compared to M3 (4.3 μg N·m −2 ·h −1 ) ( p &lt;0.05) were found. The laboratory experiment results revealed that mowing changed the soil conditions that favor the activity of denitrifiers during thawing periods. The CH 4 and N 2 O fluxes were significantly correlated with soil temperature ( p &lt;0.05). Mowing affected CH 4 uptake and N 2 O emission mainly through its effect on vegetation types and some soil properties, such as soil inorganic N content, soil temperature, and soil moisture content, while soil inorganic N and moisture were not leading factors. Our results also suggested that mowing could mitigate the potential global warming in terms of CH 4 uptake and N 2 O emissions.</description><subject>Climate change</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Emissions</subject><subject>Global warming</subject><subject>Grasslands</subject><subject>Meadows</subject><subject>Methane</subject><subject>Moisture content</subject><subject>Nitrous oxide</subject><subject>Research Article</subject><subject>Soil moisture</subject><subject>Soil properties</subject><subject>Soil temperature</subject><subject>Steppes</subject><subject>Thawing</subject><subject>Vegetation effects</subject><issn>2095-0195</issn><issn>2095-0209</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</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>eNp1kEFLAzEQhYMoWLQ_wFvAczTZZjfZo5RqC9Ve9BzSzWTdspvUZEu1v94sq-DFMJmZw_vewEPohtE7Rqm4j4wJKghlnFAuC3I6Q5OMljmhqZ__7qzML9E0xh1NT4r0-QSZhbVQ9dhb3Plj42rsHX7JNlg7g-dLjm17-ISIoWtibLyL2Abf4f4dcAfa-COJPez3gOugY2wTFQevlXMQ8LN3tW8bfY0urG4jTH_mFXp7XLzOl2S9eVrNH9akmsmiJ9qUNJdUZHpWANei4FtjLRVGVEUFFKw2xm6h0iYTeWWNMZzmWcGllIIbmc2u0O3ouw_-4wCxVzt_CC6dVKwoxVBiULFRVQUfYwCr9qHpdPhSjKohTzXmqVKeashTnRKTjUxMWldD-OP8L_QNRXt5Hg</recordid><startdate>20150901</startdate><enddate>20150901</enddate><creator>Lu, Zedong</creator><creator>Du, Rui</creator><creator>Du, Pengrui</creator><creator>Li, Ziming</creator><creator>Liang, Zongmin</creator><creator>Wang, Yaling</creator><creator>Qin, Saisai</creator><creator>Zhong, Lei</creator><general>Higher Education Press</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TG</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20150901</creationdate><title>Effect of mowing on N2O and CH4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia</title><author>Lu, Zedong ; 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Earth Sci</stitle><date>2015-09-01</date><risdate>2015</risdate><volume>9</volume><issue>3</issue><spage>473</spage><epage>486</epage><pages>473-486</pages><issn>2095-0195</issn><eissn>2095-0209</eissn><abstract>To assess the impacts of mowing on N 2 O and CH 4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia, China, two regimes were investigated: unmown since 2005 (UM), and mown once every three years since 2009 (M3). On-site measurements were conducted continuously during a year-round period (August 2011 to August 2012). During the observation period, three diurnal cycles were also measured. In addition, a targeted laboratory experiment was conducted to make up for the few measurements in winter. A large pulse of N 2 O emissions related to freeze-thaw cycles was observed at M3 during the spring thaw. Results showed that the meadow-steppes played a role as a sink for CH 4 and a source for N 2 O. Significantly lower mean CH 4 uptake at UM (40.3 μg C·m −2 ·h −1 ) as compared to M3 (70.5 μg C ·m −2 ·h −1 ) ( p &lt;0.01), and significantly higher mean N 2 O efflux at UM (6.3 μgN·m −2 ·h −1 ) as compared to M3 (4.3 μg N·m −2 ·h −1 ) ( p &lt;0.05) were found. The laboratory experiment results revealed that mowing changed the soil conditions that favor the activity of denitrifiers during thawing periods. The CH 4 and N 2 O fluxes were significantly correlated with soil temperature ( p &lt;0.05). Mowing affected CH 4 uptake and N 2 O emission mainly through its effect on vegetation types and some soil properties, such as soil inorganic N content, soil temperature, and soil moisture content, while soil inorganic N and moisture were not leading factors. Our results also suggested that mowing could mitigate the potential global warming in terms of CH 4 uptake and N 2 O emissions.</abstract><cop>Beijing</cop><pub>Higher Education Press</pub><doi>10.1007/s11707-014-0486-z</doi><tpages>14</tpages></addata></record>
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subjects Climate change
Earth and Environmental Science
Earth Sciences
Emissions
Global warming
Grasslands
Meadows
Methane
Moisture content
Nitrous oxide
Research Article
Soil moisture
Soil properties
Soil temperature
Steppes
Thawing
Vegetation effects
title Effect of mowing on N2O and CH4 fluxes emissions from the meadow-steppe grasslands of Inner Mongolia
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