Influence of macroclimate, landscape position, and management on soil organic matter in agroecosystems
We investigated patterns of soil organic matter, microbial biomass, and potential C and N mineralization in soils across landscape, regional, and management treatments in eastern Colorado. Total soil C, N, and P, microbial biomass, and C and N mineralization were highest at a northern site and on to...
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Veröffentlicht in: | Ecological applications 1995-02, Vol.5 (1), p.124-131 |
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creator | Burke, Ingrid C. Elliott, Edward T. Cole, C. Vernon |
description | We investigated patterns of soil organic matter, microbial biomass, and potential C and N mineralization in soils across landscape, regional, and management treatments in eastern Colorado. Total soil C, N, and P, microbial biomass, and C and N mineralization were highest at a northern site and on toeslope landscape positions. No-tillage and perennial grass treatments had significantly higher microbial biomass and C mineralization rates than conventional tillage treatments after only 5 yr of treatment, but only at the sites and landscape positions with high production and organic matter contents. Potential N mineralization was not different among management treatments. We suggest that a simple relationship between total soil organic matter and nutrient supply rates holds for relatively static systems represented by spatial gradients, but that transient systems undergoing losses or gains in soil organic matter may have a lag in nutrient supply responses due to immobilization dynamics. |
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Vernon</creator><creatorcontrib>Burke, Ingrid C. ; Elliott, Edward T. ; Cole, C. Vernon</creatorcontrib><description>We investigated patterns of soil organic matter, microbial biomass, and potential C and N mineralization in soils across landscape, regional, and management treatments in eastern Colorado. Total soil C, N, and P, microbial biomass, and C and N mineralization were highest at a northern site and on toeslope landscape positions. No-tillage and perennial grass treatments had significantly higher microbial biomass and C mineralization rates than conventional tillage treatments after only 5 yr of treatment, but only at the sites and landscape positions with high production and organic matter contents. Potential N mineralization was not different among management treatments. We suggest that a simple relationship between total soil organic matter and nutrient supply rates holds for relatively static systems represented by spatial gradients, but that transient systems undergoing losses or gains in soil organic matter may have a lag in nutrient supply responses due to immobilization dynamics.</description><identifier>ISSN: 1051-0761</identifier><identifier>EISSN: 1939-5582</identifier><identifier>DOI: 10.2307/1942057</identifier><language>eng</language><publisher>The Ecological Society of America</publisher><subject>Agroecosystems ; Agrology ; BIOMASA ; BIOMASS ; BIOMASSE ; CARBON ; CARBONE ; CARBONO ; CERO-LABRANZA ; CICLO BIOGEOQUIMICO ; COLORADO ; conventional tillage ; CYCLE BIOGEOCHIMIQUE ; CYCLING ; FERTILIDAD DEL SUELO ; FERTILITE DU SOL ; FLORA DEL SUELO ; FLORE DU SOL ; FOSFORO ; Grassland soils ; GRASSLANDS ; HERBAGE ; LABRANZA ; LANDSCAPE ; Landscape position ; MATERIA ORGANICA ; MATIERE ORGANIQUE ; METABOLISME DE L'AZOTE ; METABOLISMO DEL NITROGENO ; MINERALISATION ; MINERALIZACION ; MINERALIZATION ; NITROGEN CYCLE ; NITROGEN METABOLISM ; NO-TILLAGE ; NON TRAVAIL DU SOL ; ORGANIC MATTER ; Organic soils ; PAISAJE ; PAYSAGE ; perennial grassland ; PHOSPHORE ; PHOSPHORUS ; PRADERAS ; SOIL ; Soil ecology ; SOIL FERTILITY ; SOIL FLORA ; Soil nutrients ; Soil organic matter ; SOL ; SPATIAL VARIATION ; SUELO ; TILLAGE ; TRAVAIL DU SOL ; TRITICUM AESTIVUM ; ZERO TILLAGE</subject><ispartof>Ecological applications, 1995-02, Vol.5 (1), p.124-131</ispartof><rights>Copyright 1995 The Ecological Society of America</rights><rights>1995 by the Ecological Society of America</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3754-976167baa8656b4909a1483ccbe9e423402bd5f59332825814c7cf17b6cad3b63</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1942057$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1942057$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27923,27924,58016,58249</link.rule.ids></links><search><creatorcontrib>Burke, Ingrid C.</creatorcontrib><creatorcontrib>Elliott, Edward T.</creatorcontrib><creatorcontrib>Cole, C. Vernon</creatorcontrib><title>Influence of macroclimate, landscape position, and management on soil organic matter in agroecosystems</title><title>Ecological applications</title><description>We investigated patterns of soil organic matter, microbial biomass, and potential C and N mineralization in soils across landscape, regional, and management treatments in eastern Colorado. Total soil C, N, and P, microbial biomass, and C and N mineralization were highest at a northern site and on toeslope landscape positions. No-tillage and perennial grass treatments had significantly higher microbial biomass and C mineralization rates than conventional tillage treatments after only 5 yr of treatment, but only at the sites and landscape positions with high production and organic matter contents. Potential N mineralization was not different among management treatments. We suggest that a simple relationship between total soil organic matter and nutrient supply rates holds for relatively static systems represented by spatial gradients, but that transient systems undergoing losses or gains in soil organic matter may have a lag in nutrient supply responses due to immobilization dynamics.</description><subject>Agroecosystems</subject><subject>Agrology</subject><subject>BIOMASA</subject><subject>BIOMASS</subject><subject>BIOMASSE</subject><subject>CARBON</subject><subject>CARBONE</subject><subject>CARBONO</subject><subject>CERO-LABRANZA</subject><subject>CICLO BIOGEOQUIMICO</subject><subject>COLORADO</subject><subject>conventional tillage</subject><subject>CYCLE BIOGEOCHIMIQUE</subject><subject>CYCLING</subject><subject>FERTILIDAD DEL SUELO</subject><subject>FERTILITE DU SOL</subject><subject>FLORA DEL SUELO</subject><subject>FLORE DU SOL</subject><subject>FOSFORO</subject><subject>Grassland soils</subject><subject>GRASSLANDS</subject><subject>HERBAGE</subject><subject>LABRANZA</subject><subject>LANDSCAPE</subject><subject>Landscape position</subject><subject>MATERIA ORGANICA</subject><subject>MATIERE ORGANIQUE</subject><subject>METABOLISME DE L'AZOTE</subject><subject>METABOLISMO DEL NITROGENO</subject><subject>MINERALISATION</subject><subject>MINERALIZACION</subject><subject>MINERALIZATION</subject><subject>NITROGEN CYCLE</subject><subject>NITROGEN METABOLISM</subject><subject>NO-TILLAGE</subject><subject>NON TRAVAIL DU SOL</subject><subject>ORGANIC MATTER</subject><subject>Organic soils</subject><subject>PAISAJE</subject><subject>PAYSAGE</subject><subject>perennial grassland</subject><subject>PHOSPHORE</subject><subject>PHOSPHORUS</subject><subject>PRADERAS</subject><subject>SOIL</subject><subject>Soil ecology</subject><subject>SOIL FERTILITY</subject><subject>SOIL FLORA</subject><subject>Soil nutrients</subject><subject>Soil organic matter</subject><subject>SOL</subject><subject>SPATIAL VARIATION</subject><subject>SUELO</subject><subject>TILLAGE</subject><subject>TRAVAIL DU SOL</subject><subject>TRITICUM AESTIVUM</subject><subject>ZERO TILLAGE</subject><issn>1051-0761</issn><issn>1939-5582</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1995</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LxDAQhosoqKt495SD6MVqvtMcZVk_QFBQzyHNTpdIm6xJF9l_b6Re1VwmZJ55mTxVdULwFWVYXRPNKRZqpzogmulaiIbuljsWpMZKkv3qMOd3XA6l9KDqHkLXbyA4QLFDg3Uput4PdoRL1NuwzM6uAa1j9qOP4RKVp0IFu4IBwohiQDn6HsW0ssG70hpHSMgHZFcpgot5m0cY8lG119k-w_FPnVVvt4vX-X39-HT3ML95rB1Tgte6LChVa20jhWy5xtoS3jDnWtDAKeOYtkvRCc0YbahoCHfKdUS10tklayWbVedT7jrFjw3k0Qw-O-jLVyBusiENUarh-H9QKiYbpgt4MYHFTM4JOrNOxU_aGoLNt3DzI7yQZCI_fQ_b3zCzuHkmWgtBCOVl5myaec9jTH9En05YZ6MpZn02by8lQ2LJ2ReZR5QZ</recordid><startdate>199502</startdate><enddate>199502</enddate><creator>Burke, Ingrid C.</creator><creator>Elliott, Edward T.</creator><creator>Cole, C. Vernon</creator><general>The Ecological Society of America</general><general>Ecological Society of America</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>C1K</scope><scope>7TG</scope><scope>KL.</scope></search><sort><creationdate>199502</creationdate><title>Influence of macroclimate, landscape position, and management on soil organic matter in agroecosystems</title><author>Burke, Ingrid C. ; Elliott, Edward T. ; Cole, C. Vernon</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3754-976167baa8656b4909a1483ccbe9e423402bd5f59332825814c7cf17b6cad3b63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1995</creationdate><topic>Agroecosystems</topic><topic>Agrology</topic><topic>BIOMASA</topic><topic>BIOMASS</topic><topic>BIOMASSE</topic><topic>CARBON</topic><topic>CARBONE</topic><topic>CARBONO</topic><topic>CERO-LABRANZA</topic><topic>CICLO BIOGEOQUIMICO</topic><topic>COLORADO</topic><topic>conventional tillage</topic><topic>CYCLE BIOGEOCHIMIQUE</topic><topic>CYCLING</topic><topic>FERTILIDAD DEL SUELO</topic><topic>FERTILITE DU SOL</topic><topic>FLORA DEL SUELO</topic><topic>FLORE DU SOL</topic><topic>FOSFORO</topic><topic>Grassland soils</topic><topic>GRASSLANDS</topic><topic>HERBAGE</topic><topic>LABRANZA</topic><topic>LANDSCAPE</topic><topic>Landscape position</topic><topic>MATERIA ORGANICA</topic><topic>MATIERE ORGANIQUE</topic><topic>METABOLISME DE L'AZOTE</topic><topic>METABOLISMO DEL NITROGENO</topic><topic>MINERALISATION</topic><topic>MINERALIZACION</topic><topic>MINERALIZATION</topic><topic>NITROGEN CYCLE</topic><topic>NITROGEN METABOLISM</topic><topic>NO-TILLAGE</topic><topic>NON TRAVAIL DU SOL</topic><topic>ORGANIC MATTER</topic><topic>Organic soils</topic><topic>PAISAJE</topic><topic>PAYSAGE</topic><topic>perennial grassland</topic><topic>PHOSPHORE</topic><topic>PHOSPHORUS</topic><topic>PRADERAS</topic><topic>SOIL</topic><topic>Soil ecology</topic><topic>SOIL FERTILITY</topic><topic>SOIL FLORA</topic><topic>Soil nutrients</topic><topic>Soil organic matter</topic><topic>SOL</topic><topic>SPATIAL VARIATION</topic><topic>SUELO</topic><topic>TILLAGE</topic><topic>TRAVAIL DU SOL</topic><topic>TRITICUM AESTIVUM</topic><topic>ZERO TILLAGE</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Burke, Ingrid C.</creatorcontrib><creatorcontrib>Elliott, Edward T.</creatorcontrib><creatorcontrib>Cole, C. Vernon</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Ecological applications</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Burke, Ingrid C.</au><au>Elliott, Edward T.</au><au>Cole, C. Vernon</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of macroclimate, landscape position, and management on soil organic matter in agroecosystems</atitle><jtitle>Ecological applications</jtitle><date>1995-02</date><risdate>1995</risdate><volume>5</volume><issue>1</issue><spage>124</spage><epage>131</epage><pages>124-131</pages><issn>1051-0761</issn><eissn>1939-5582</eissn><abstract>We investigated patterns of soil organic matter, microbial biomass, and potential C and N mineralization in soils across landscape, regional, and management treatments in eastern Colorado. Total soil C, N, and P, microbial biomass, and C and N mineralization were highest at a northern site and on toeslope landscape positions. No-tillage and perennial grass treatments had significantly higher microbial biomass and C mineralization rates than conventional tillage treatments after only 5 yr of treatment, but only at the sites and landscape positions with high production and organic matter contents. Potential N mineralization was not different among management treatments. We suggest that a simple relationship between total soil organic matter and nutrient supply rates holds for relatively static systems represented by spatial gradients, but that transient systems undergoing losses or gains in soil organic matter may have a lag in nutrient supply responses due to immobilization dynamics.</abstract><pub>The Ecological Society of America</pub><doi>10.2307/1942057</doi><tpages>8</tpages></addata></record> |
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subjects | Agroecosystems Agrology BIOMASA BIOMASS BIOMASSE CARBON CARBONE CARBONO CERO-LABRANZA CICLO BIOGEOQUIMICO COLORADO conventional tillage CYCLE BIOGEOCHIMIQUE CYCLING FERTILIDAD DEL SUELO FERTILITE DU SOL FLORA DEL SUELO FLORE DU SOL FOSFORO Grassland soils GRASSLANDS HERBAGE LABRANZA LANDSCAPE Landscape position MATERIA ORGANICA MATIERE ORGANIQUE METABOLISME DE L'AZOTE METABOLISMO DEL NITROGENO MINERALISATION MINERALIZACION MINERALIZATION NITROGEN CYCLE NITROGEN METABOLISM NO-TILLAGE NON TRAVAIL DU SOL ORGANIC MATTER Organic soils PAISAJE PAYSAGE perennial grassland PHOSPHORE PHOSPHORUS PRADERAS SOIL Soil ecology SOIL FERTILITY SOIL FLORA Soil nutrients Soil organic matter SOL SPATIAL VARIATION SUELO TILLAGE TRAVAIL DU SOL TRITICUM AESTIVUM ZERO TILLAGE |
title | Influence of macroclimate, landscape position, and management on soil organic matter in agroecosystems |
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