Differences in the Spatial Variability Among CO2, CH4, and N2O Gas Fluxes from an Urban Forest Soil in Japan
The spatial variability of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) fluxes from forest soil with high nitrogen (N) deposition was investigated at a rolling hill region in Japan. Gas fluxes were measured on July 25th and December 5th, 2008 at 100 points within a 100 × 100 m grid....
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| Veröffentlicht in: | Ambio 2015-02, Vol.44 (1), p.55-66 |
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| creator | Bellingrath-Kimura, Sonoko Dorothea Kishimoto-Mo, Ayaka Wenhong Oura, Noriko Sekikawa, Seiko Yonemura, Seichiro Sudo, Shigeto Hayakawa, Atsushi Minamikawa, Kazunori Takata, Yusuke Hara, Hiroshi |
| description | The spatial variability of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) fluxes from forest soil with high nitrogen (N) deposition was investigated at a rolling hill region in Japan. Gas fluxes were measured on July 25th and December 5th, 2008 at 100 points within a 100 × 100 m grid. Slope direction and position influenced soil characteristics and site-specific emissions were found. The CO2 flux showed no topological difference in July, but was significantly lower in December for north-slope with coniferous trees. Spatial dependency of CH4 fluxes was stronger than that of CO2 or N2O and showed a significantly higher uptake in hill top, and emissions in the valley indicating strong influence of water status. N2O fluxes showed no spatial dependency and exhibited high hot spots at different topology in July and December. The high N deposition led to high N2O fluxes and emphasized the spatial variability. |
| doi_str_mv | 10.1007/s13280-014-0521-z |
| format | Article |
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Gas fluxes were measured on July 25th and December 5th, 2008 at 100 points within a 100 × 100 m grid. Slope direction and position influenced soil characteristics and site-specific emissions were found. The CO2 flux showed no topological difference in July, but was significantly lower in December for north-slope with coniferous trees. Spatial dependency of CH4 fluxes was stronger than that of CO2 or N2O and showed a significantly higher uptake in hill top, and emissions in the valley indicating strong influence of water status. N2O fluxes showed no spatial dependency and exhibited high hot spots at different topology in July and December. The high N deposition led to high N2O fluxes and emphasized the spatial variability.</description><identifier>ISSN: 0044-7447</identifier><identifier>EISSN: 1654-7209</identifier><identifier>DOI: 10.1007/s13280-014-0521-z</identifier><identifier>PMID: 24736940</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Atmospheric Sciences ; Biogeochemistry ; Carbon dioxide ; Climate change ; Coniferous trees ; Deposition ; Earth and Environmental Science ; Ecology ; Emissions ; Environment ; Environmental Engineering/Biotechnology ; Environmental Management ; Fluxes ; Forest soils ; Forests ; Methane ; Nitrous oxide ; Nitrous oxides ; Physical Geography ; Soil (material) ; Soil characteristics ; Spatial dependencies ; Topography ; Topology ; Urban areas ; Urban forests ; Valleys</subject><ispartof>Ambio, 2015-02, Vol.44 (1), p.55-66</ispartof><rights>2015 Royal Swedish Academy of Sciences</rights><rights>Royal Swedish Academy of Sciences 2014</rights><rights>Royal Swedish Academy of Sciences 2015</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-b660t-4244a69e14ee8bc333af6b4cfb4e5c5f86ed8b154c78a3a50a9192d5cd0a6bb53</citedby><cites>FETCH-LOGICAL-b660t-4244a69e14ee8bc333af6b4cfb4e5c5f86ed8b154c78a3a50a9192d5cd0a6bb53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/24670725$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/24670725$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,723,776,780,799,881,27901,27902,41464,42533,51294,53766,53768,57992,58225</link.rule.ids></links><search><creatorcontrib>Bellingrath-Kimura, Sonoko Dorothea</creatorcontrib><creatorcontrib>Kishimoto-Mo, Ayaka Wenhong</creatorcontrib><creatorcontrib>Oura, Noriko</creatorcontrib><creatorcontrib>Sekikawa, Seiko</creatorcontrib><creatorcontrib>Yonemura, Seichiro</creatorcontrib><creatorcontrib>Sudo, Shigeto</creatorcontrib><creatorcontrib>Hayakawa, Atsushi</creatorcontrib><creatorcontrib>Minamikawa, Kazunori</creatorcontrib><creatorcontrib>Takata, Yusuke</creatorcontrib><creatorcontrib>Hara, Hiroshi</creatorcontrib><title>Differences in the Spatial Variability Among CO2, CH4, and N2O Gas Fluxes from an Urban Forest Soil in Japan</title><title>Ambio</title><addtitle>AMBIO</addtitle><description>The spatial variability of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) fluxes from forest soil with high nitrogen (N) deposition was investigated at a rolling hill region in Japan. Gas fluxes were measured on July 25th and December 5th, 2008 at 100 points within a 100 × 100 m grid. Slope direction and position influenced soil characteristics and site-specific emissions were found. The CO2 flux showed no topological difference in July, but was significantly lower in December for north-slope with coniferous trees. Spatial dependency of CH4 fluxes was stronger than that of CO2 or N2O and showed a significantly higher uptake in hill top, and emissions in the valley indicating strong influence of water status. N2O fluxes showed no spatial dependency and exhibited high hot spots at different topology in July and December. The high N deposition led to high N2O fluxes and emphasized the spatial variability.</description><subject>Atmospheric Sciences</subject><subject>Biogeochemistry</subject><subject>Carbon dioxide</subject><subject>Climate change</subject><subject>Coniferous trees</subject><subject>Deposition</subject><subject>Earth and Environmental Science</subject><subject>Ecology</subject><subject>Emissions</subject><subject>Environment</subject><subject>Environmental Engineering/Biotechnology</subject><subject>Environmental Management</subject><subject>Fluxes</subject><subject>Forest soils</subject><subject>Forests</subject><subject>Methane</subject><subject>Nitrous oxide</subject><subject>Nitrous oxides</subject><subject>Physical Geography</subject><subject>Soil (material)</subject><subject>Soil characteristics</subject><subject>Spatial dependencies</subject><subject>Topography</subject><subject>Topology</subject><subject>Urban areas</subject><subject>Urban 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Hiroshi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Differences in the Spatial Variability Among CO2, CH4, and N2O Gas Fluxes from an Urban Forest Soil in Japan</atitle><jtitle>Ambio</jtitle><stitle>AMBIO</stitle><date>2015-02-01</date><risdate>2015</risdate><volume>44</volume><issue>1</issue><spage>55</spage><epage>66</epage><pages>55-66</pages><issn>0044-7447</issn><eissn>1654-7209</eissn><abstract>The spatial variability of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) fluxes from forest soil with high nitrogen (N) deposition was investigated at a rolling hill region in Japan. Gas fluxes were measured on July 25th and December 5th, 2008 at 100 points within a 100 × 100 m grid. Slope direction and position influenced soil characteristics and site-specific emissions were found. The CO2 flux showed no topological difference in July, but was significantly lower in December for north-slope with coniferous trees. Spatial dependency of CH4 fluxes was stronger than that of CO2 or N2O and showed a significantly higher uptake in hill top, and emissions in the valley indicating strong influence of water status. N2O fluxes showed no spatial dependency and exhibited high hot spots at different topology in July and December. The high N deposition led to high N2O fluxes and emphasized the spatial variability.</abstract><cop>Dordrecht</cop><pub>Springer</pub><pmid>24736940</pmid><doi>10.1007/s13280-014-0521-z</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Atmospheric Sciences Biogeochemistry Carbon dioxide Climate change Coniferous trees Deposition Earth and Environmental Science Ecology Emissions Environment Environmental Engineering/Biotechnology Environmental Management Fluxes Forest soils Forests Methane Nitrous oxide Nitrous oxides Physical Geography Soil (material) Soil characteristics Spatial dependencies Topography Topology Urban areas Urban forests Valleys |
| title | Differences in the Spatial Variability Among CO2, CH4, and N2O Gas Fluxes from an Urban Forest Soil in Japan |
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