Effects of land use change on soil carbon cycling in the conterminous United States from 1900 to 2050
We developed matrices representing historical area transitions between forest and other land uses. We projected future transitions on the basis of historical transitions and econometric model results. These matrices were used to drive a model of changes in soil and forest floor carbon stocks. Our mo...
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| Veröffentlicht in: | Global biogeochemical cycles 2007-09, Vol.21 (3), p.n/a |
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| creator | Woodbury, P.B Heath, L.S Smith, J.E |
| description | We developed matrices representing historical area transitions between forest and other land uses. We projected future transitions on the basis of historical transitions and econometric model results. These matrices were used to drive a model of changes in soil and forest floor carbon stocks. Our model predicted net carbon emission from 1900 until 1982, then sequestration until 2030, with little subsequent change. However, the northeast region showed substantial carbon sequestration from 1900 to the present. From 1990 to 2004, afforestation caused sequestration averaging 17 Tg C yr−1: 6 Tg C yr−1 in soil and 11 Tg C yr−1 in forest floor. Deforestation caused emission averaging 12 Tg C yr−1: 3 Tg C yr−1 from soil and 9 Tg C yr−1 from forest floor. However, these effects were only 5% of the total change in carbon stocks in all forestland. |
| doi_str_mv | 10.1029/2007GB002950 |
| format | Article |
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We projected future transitions on the basis of historical transitions and econometric model results. These matrices were used to drive a model of changes in soil and forest floor carbon stocks. Our model predicted net carbon emission from 1900 until 1982, then sequestration until 2030, with little subsequent change. However, the northeast region showed substantial carbon sequestration from 1900 to the present. From 1990 to 2004, afforestation caused sequestration averaging 17 Tg C yr−1: 6 Tg C yr−1 in soil and 11 Tg C yr−1 in forest floor. Deforestation caused emission averaging 12 Tg C yr−1: 3 Tg C yr−1 from soil and 9 Tg C yr−1 from forest floor. However, these effects were only 5% of the total change in carbon stocks in all forestland.</description><identifier>ISSN: 0886-6236</identifier><identifier>EISSN: 1944-9224</identifier><identifier>DOI: 10.1029/2007GB002950</identifier><identifier>CODEN: GBCYEP</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>afforestation ; agricultural land ; Animal and plant ecology ; Animal, plant and microbial ecology ; biodegradation ; biogeochemical cycles ; Biological and medical sciences ; carbon budget ; carbon dioxide ; carbon sequestration ; deforestation ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; forest soils ; Fundamental and applied biological sciences. Psychology ; gas emissions ; General aspects ; Geochemistry ; grasslands ; land use change ; soil organic carbon ; soil organic matter ; soil respiration ; Synecology</subject><ispartof>Global biogeochemical cycles, 2007-09, Vol.21 (3), p.n/a</ispartof><rights>Copyright 2007 by the American Geophysical Union.</rights><rights>2007 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4387-d3fb57a536e2114d16722c1da5595f8e33deb5f539903536a8b0ea6795108c403</citedby><cites>FETCH-LOGICAL-c4387-d3fb57a536e2114d16722c1da5595f8e33deb5f539903536a8b0ea6795108c403</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2007GB002950$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2007GB002950$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=19193452$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Woodbury, P.B</creatorcontrib><creatorcontrib>Heath, L.S</creatorcontrib><creatorcontrib>Smith, J.E</creatorcontrib><title>Effects of land use change on soil carbon cycling in the conterminous United States from 1900 to 2050</title><title>Global biogeochemical cycles</title><addtitle>Global Biogeochem. Cycles</addtitle><description>We developed matrices representing historical area transitions between forest and other land uses. We projected future transitions on the basis of historical transitions and econometric model results. These matrices were used to drive a model of changes in soil and forest floor carbon stocks. Our model predicted net carbon emission from 1900 until 1982, then sequestration until 2030, with little subsequent change. However, the northeast region showed substantial carbon sequestration from 1900 to the present. From 1990 to 2004, afforestation caused sequestration averaging 17 Tg C yr−1: 6 Tg C yr−1 in soil and 11 Tg C yr−1 in forest floor. Deforestation caused emission averaging 12 Tg C yr−1: 3 Tg C yr−1 from soil and 9 Tg C yr−1 from forest floor. However, these effects were only 5% of the total change in carbon stocks in all forestland.</description><subject>afforestation</subject><subject>agricultural land</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>biodegradation</subject><subject>biogeochemical cycles</subject><subject>Biological and medical sciences</subject><subject>carbon budget</subject><subject>carbon dioxide</subject><subject>carbon sequestration</subject><subject>deforestation</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>forest soils</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>gas emissions</subject><subject>General aspects</subject><subject>Geochemistry</subject><subject>grasslands</subject><subject>land use change</subject><subject>soil organic carbon</subject><subject>soil organic matter</subject><subject>soil respiration</subject><subject>Synecology</subject><issn>0886-6236</issn><issn>1944-9224</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNp9kc1vEzEQxVcIJELhxh1f4MSW8dfu-khDSZEiEJQUiYvleMepYWO3tiPIf4_RVsCJ08zh957evGmapxROKTD1igH0qzOoq4R7zYIqIVrFmLjfLGAYurZjvHvYPMr5GwAVUqpFg-fOoS2ZREcmE0ZyyEjstQk7JDGQHP1ErEnbutujnXzYER9Iua5QDAXT3od4yGQTfMGRXBZTMBOX4p5QBUBKJAwkPG4eODNlfHI3T5rN2_PPy4t2_WH1bvl63VrBh74dudvK3kjeIaNUjLTrGbN0NDWqdANyPuJWOsmVAl4pM2wBTdcrSWGwAvhJ82L2vUnx9oC56L3PFqd6GdaYmoEYlOKigi9n0KaYc0Knb5Lfm3TUFPTvLvW_XVb8-Z2vydZMLplgff6rUbSaSlY5OnM__ITH_3rq1dmSctVXTTtrfC7484_GpO-663kv9Zf3K31Fr76uP8o3-lPln828M1GbXao5NpcMKIf645pE8F8fyZdX</recordid><startdate>200709</startdate><enddate>200709</enddate><creator>Woodbury, P.B</creator><creator>Heath, L.S</creator><creator>Smith, J.E</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>FBQ</scope><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7ST</scope><scope>7TV</scope><scope>7U6</scope><scope>C1K</scope></search><sort><creationdate>200709</creationdate><title>Effects of land use change on soil carbon cycling in the conterminous United States from 1900 to 2050</title><author>Woodbury, P.B ; Heath, L.S ; Smith, J.E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4387-d3fb57a536e2114d16722c1da5595f8e33deb5f539903536a8b0ea6795108c403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>afforestation</topic><topic>agricultural land</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>biodegradation</topic><topic>biogeochemical cycles</topic><topic>Biological and medical sciences</topic><topic>carbon budget</topic><topic>carbon dioxide</topic><topic>carbon sequestration</topic><topic>deforestation</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>forest soils</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>gas emissions</topic><topic>General aspects</topic><topic>Geochemistry</topic><topic>grasslands</topic><topic>land use change</topic><topic>soil organic carbon</topic><topic>soil organic matter</topic><topic>soil respiration</topic><topic>Synecology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Woodbury, P.B</creatorcontrib><creatorcontrib>Heath, L.S</creatorcontrib><creatorcontrib>Smith, J.E</creatorcontrib><collection>AGRIS</collection><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Pollution Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Global biogeochemical cycles</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Woodbury, P.B</au><au>Heath, L.S</au><au>Smith, J.E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effects of land use change on soil carbon cycling in the conterminous United States from 1900 to 2050</atitle><jtitle>Global biogeochemical cycles</jtitle><addtitle>Global Biogeochem. Cycles</addtitle><date>2007-09</date><risdate>2007</risdate><volume>21</volume><issue>3</issue><epage>n/a</epage><issn>0886-6236</issn><eissn>1944-9224</eissn><coden>GBCYEP</coden><abstract>We developed matrices representing historical area transitions between forest and other land uses. We projected future transitions on the basis of historical transitions and econometric model results. These matrices were used to drive a model of changes in soil and forest floor carbon stocks. Our model predicted net carbon emission from 1900 until 1982, then sequestration until 2030, with little subsequent change. However, the northeast region showed substantial carbon sequestration from 1900 to the present. From 1990 to 2004, afforestation caused sequestration averaging 17 Tg C yr−1: 6 Tg C yr−1 in soil and 11 Tg C yr−1 in forest floor. Deforestation caused emission averaging 12 Tg C yr−1: 3 Tg C yr−1 from soil and 9 Tg C yr−1 from forest floor. However, these effects were only 5% of the total change in carbon stocks in all forestland.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2007GB002950</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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| source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | afforestation agricultural land Animal and plant ecology Animal, plant and microbial ecology biodegradation biogeochemical cycles Biological and medical sciences carbon budget carbon dioxide carbon sequestration deforestation Earth sciences Earth, ocean, space Exact sciences and technology forest soils Fundamental and applied biological sciences. Psychology gas emissions General aspects Geochemistry grasslands land use change soil organic carbon soil organic matter soil respiration Synecology |
| title | Effects of land use change on soil carbon cycling in the conterminous United States from 1900 to 2050 |
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