Free and intra-aggregate organic matter as indicators of soil quality change in volcanic soils under contrasting crop rotations
Soil physical fractionation techniques may provide indicators of changing soil organic carbon (SOC) content; however, they have not been widely tested on volcanic soils (Andisols). In this study, we assessed two fractions as potential indicators in volcanic soils, using two sites in Chile converted...
Gespeichert in:
| Veröffentlicht in: | Soil use and management 2013-12, Vol.29 (4), p.531-539 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 539 |
|---|---|
| container_issue | 4 |
| container_start_page | 531 |
| container_title | Soil use and management |
| container_volume | 29 |
| creator | Zagal, E. Córdova, C. Sohi, S. P. Powlson, D. S. |
| description | Soil physical fractionation techniques may provide indicators of changing soil organic carbon (SOC) content; however, they have not been widely tested on volcanic soils (Andisols). In this study, we assessed two fractions as potential indicators in volcanic soils, using two sites in Chile converted from natural grassland to arable and mixed crop rotations, 8 and 16 yr previously. In the 8‐yr experiment, SOC had declined under all rotations, with smaller changes where the rotation included 3 or 5 yr of perennial pasture. Whereas the average SOC was only 76% of the level in the preceding natural grassland, the corresponding value after 16 yr for the second site was 98% (and 93% under continuous arable), probably reflecting its high allophane clay content. The fractionation procedure tested proved applicable to both Andisols, but the intra‐aggregate light fraction (IA‐SOM, isolated in sodium iodide solution at 1.80 g/cm3 after ultrasonic dispersion) accounted for a very small proportion of total SOC ( |
| doi_str_mv | 10.1111/sum.12070 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1475548813</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3144553081</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3980-ba2463ad56e90c1aec73b28a07c80af5ea89db7ca39512f25bd8f45c45196a053</originalsourceid><addsrcrecordid>eNp1kU1PFTEUhidGE6_own_QxJjoYqCf087SEEACSIyCxk1zbqczFue2l7aj3BV_3Q4XWJjYzVn0eZ-c9q2q1wTvknL20rTaJRRL_KRaEC5FTSVnT6sFpk1TY8zo8-pFSlcYUyIbvKhuD6O1CHyHnM8RahiGaAfIFoU4gHcGrSBnGxGkQnTOQA4xodCjFNyIricYXd4g8xP8YAuBfofR3OXm-4Qm35WwCbM8ZecHZGJYoxgyZBd8elk962FM9tX93KkuDg--7n-sT8-Pjvc_nNaGtQrXS6C8YdCJxrbYELBGsiVVgKVRGHphQbXdUhpgrSC0p2LZqZ4LwwVpG8CC7VTvtt51DNeTTVmvXDJ2HMHbMCU9_5XgShFW0Df_oFdhir5sV6iGC04Y5YV6v6XKe1KKttfr6FYQN5pgPVehSxX6rorCvr03QjIw9hG8cekxQBXGjZCzc2_L_XGj3fxfqL9cnD2Y623CpWxvHhMQf-lGMin0t09H-uzH5edL9f1Et-wvlsyosg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1464541324</pqid></control><display><type>article</type><title>Free and intra-aggregate organic matter as indicators of soil quality change in volcanic soils under contrasting crop rotations</title><source>Wiley Online Library All Journals</source><creator>Zagal, E. ; Córdova, C. ; Sohi, S. P. ; Powlson, D. S.</creator><creatorcontrib>Zagal, E. ; Córdova, C. ; Sohi, S. P. ; Powlson, D. S.</creatorcontrib><description>Soil physical fractionation techniques may provide indicators of changing soil organic carbon (SOC) content; however, they have not been widely tested on volcanic soils (Andisols). In this study, we assessed two fractions as potential indicators in volcanic soils, using two sites in Chile converted from natural grassland to arable and mixed crop rotations, 8 and 16 yr previously. In the 8‐yr experiment, SOC had declined under all rotations, with smaller changes where the rotation included 3 or 5 yr of perennial pasture. Whereas the average SOC was only 76% of the level in the preceding natural grassland, the corresponding value after 16 yr for the second site was 98% (and 93% under continuous arable), probably reflecting its high allophane clay content. The fractionation procedure tested proved applicable to both Andisols, but the intra‐aggregate light fraction (IA‐SOM, isolated in sodium iodide solution at 1.80 g/cm3 after ultrasonic dispersion) accounted for a very small proportion of total SOC (<1%). We suggest that in Andisols, the free light fraction (FR‐SOM, isolated in sodium iodide at solution of the same density, but prior to ultrasonic dispersion) is stabilised to a greater extent than in nonvolcanic soils, and the intra‐aggregate fraction plays a more minor role as a pool of intermediate turnover. The relative value of each fraction needs to be confirmed through dynamic experiments, using more sites, and including situations where SOC content is initially low.</description><identifier>ISSN: 0266-0032</identifier><identifier>EISSN: 1475-2743</identifier><identifier>DOI: 10.1111/sum.12070</identifier><identifier>CODEN: SUMAEU</identifier><language>eng</language><publisher>Oxford: Blackwell Publishing Ltd</publisher><subject>Agronomy. Soil science and plant productions ; Andisols ; arable ; Arable land ; Biological and medical sciences ; Chemical, physicochemical, biochemical and biological properties ; Cropping systems. Cultivation. Soil tillage ; Density ; Dispersions ; Fractionation ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Generalities. Cropping systems and patterns ; Grasslands ; Indicators ; NaI ; Organic matter ; pasture ; physical fractionation ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Soil (material) ; soil organic matter ; Soil science ; Volcanic soils</subject><ispartof>Soil use and management, 2013-12, Vol.29 (4), p.531-539</ispartof><rights>2013 The Authors. Journal compilation © 2013 British Society of Soil Science</rights><rights>2015 INIST-CNRS</rights><rights>Journal compilation © 2013 British Society of Soil Science</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3980-ba2463ad56e90c1aec73b28a07c80af5ea89db7ca39512f25bd8f45c45196a053</citedby><cites>FETCH-LOGICAL-c3980-ba2463ad56e90c1aec73b28a07c80af5ea89db7ca39512f25bd8f45c45196a053</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fsum.12070$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fsum.12070$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27923,27924,45573,45574</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28006574$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Zagal, E.</creatorcontrib><creatorcontrib>Córdova, C.</creatorcontrib><creatorcontrib>Sohi, S. P.</creatorcontrib><creatorcontrib>Powlson, D. S.</creatorcontrib><title>Free and intra-aggregate organic matter as indicators of soil quality change in volcanic soils under contrasting crop rotations</title><title>Soil use and management</title><addtitle>Soil Use Manage</addtitle><description>Soil physical fractionation techniques may provide indicators of changing soil organic carbon (SOC) content; however, they have not been widely tested on volcanic soils (Andisols). In this study, we assessed two fractions as potential indicators in volcanic soils, using two sites in Chile converted from natural grassland to arable and mixed crop rotations, 8 and 16 yr previously. In the 8‐yr experiment, SOC had declined under all rotations, with smaller changes where the rotation included 3 or 5 yr of perennial pasture. Whereas the average SOC was only 76% of the level in the preceding natural grassland, the corresponding value after 16 yr for the second site was 98% (and 93% under continuous arable), probably reflecting its high allophane clay content. The fractionation procedure tested proved applicable to both Andisols, but the intra‐aggregate light fraction (IA‐SOM, isolated in sodium iodide solution at 1.80 g/cm3 after ultrasonic dispersion) accounted for a very small proportion of total SOC (<1%). We suggest that in Andisols, the free light fraction (FR‐SOM, isolated in sodium iodide at solution of the same density, but prior to ultrasonic dispersion) is stabilised to a greater extent than in nonvolcanic soils, and the intra‐aggregate fraction plays a more minor role as a pool of intermediate turnover. The relative value of each fraction needs to be confirmed through dynamic experiments, using more sites, and including situations where SOC content is initially low.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Andisols</subject><subject>arable</subject><subject>Arable land</subject><subject>Biological and medical sciences</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>Cropping systems. Cultivation. Soil tillage</subject><subject>Density</subject><subject>Dispersions</subject><subject>Fractionation</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Generalities. Cropping systems and patterns</subject><subject>Grasslands</subject><subject>Indicators</subject><subject>NaI</subject><subject>Organic matter</subject><subject>pasture</subject><subject>physical fractionation</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Soil (material)</subject><subject>soil organic matter</subject><subject>Soil science</subject><subject>Volcanic soils</subject><issn>0266-0032</issn><issn>1475-2743</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNp1kU1PFTEUhidGE6_own_QxJjoYqCf087SEEACSIyCxk1zbqczFue2l7aj3BV_3Q4XWJjYzVn0eZ-c9q2q1wTvknL20rTaJRRL_KRaEC5FTSVnT6sFpk1TY8zo8-pFSlcYUyIbvKhuD6O1CHyHnM8RahiGaAfIFoU4gHcGrSBnGxGkQnTOQA4xodCjFNyIricYXd4g8xP8YAuBfofR3OXm-4Qm35WwCbM8ZecHZGJYoxgyZBd8elk962FM9tX93KkuDg--7n-sT8-Pjvc_nNaGtQrXS6C8YdCJxrbYELBGsiVVgKVRGHphQbXdUhpgrSC0p2LZqZ4LwwVpG8CC7VTvtt51DNeTTVmvXDJ2HMHbMCU9_5XgShFW0Df_oFdhir5sV6iGC04Y5YV6v6XKe1KKttfr6FYQN5pgPVehSxX6rorCvr03QjIw9hG8cekxQBXGjZCzc2_L_XGj3fxfqL9cnD2Y623CpWxvHhMQf-lGMin0t09H-uzH5edL9f1Et-wvlsyosg</recordid><startdate>201312</startdate><enddate>201312</enddate><creator>Zagal, E.</creator><creator>Córdova, C.</creator><creator>Sohi, S. P.</creator><creator>Powlson, D. S.</creator><general>Blackwell Publishing Ltd</general><general>Wiley-Blackwell</general><general>Wiley Subscription Services, Inc</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>201312</creationdate><title>Free and intra-aggregate organic matter as indicators of soil quality change in volcanic soils under contrasting crop rotations</title><author>Zagal, E. ; Córdova, C. ; Sohi, S. P. ; Powlson, D. S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3980-ba2463ad56e90c1aec73b28a07c80af5ea89db7ca39512f25bd8f45c45196a053</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Andisols</topic><topic>arable</topic><topic>Arable land</topic><topic>Biological and medical sciences</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>Cropping systems. Cultivation. Soil tillage</topic><topic>Density</topic><topic>Dispersions</topic><topic>Fractionation</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>Generalities. Cropping systems and patterns</topic><topic>Grasslands</topic><topic>Indicators</topic><topic>NaI</topic><topic>Organic matter</topic><topic>pasture</topic><topic>physical fractionation</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Soil (material)</topic><topic>soil organic matter</topic><topic>Soil science</topic><topic>Volcanic soils</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zagal, E.</creatorcontrib><creatorcontrib>Córdova, C.</creatorcontrib><creatorcontrib>Sohi, S. P.</creatorcontrib><creatorcontrib>Powlson, D. S.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Soil use and management</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zagal, E.</au><au>Córdova, C.</au><au>Sohi, S. P.</au><au>Powlson, D. S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Free and intra-aggregate organic matter as indicators of soil quality change in volcanic soils under contrasting crop rotations</atitle><jtitle>Soil use and management</jtitle><addtitle>Soil Use Manage</addtitle><date>2013-12</date><risdate>2013</risdate><volume>29</volume><issue>4</issue><spage>531</spage><epage>539</epage><pages>531-539</pages><issn>0266-0032</issn><eissn>1475-2743</eissn><coden>SUMAEU</coden><abstract>Soil physical fractionation techniques may provide indicators of changing soil organic carbon (SOC) content; however, they have not been widely tested on volcanic soils (Andisols). In this study, we assessed two fractions as potential indicators in volcanic soils, using two sites in Chile converted from natural grassland to arable and mixed crop rotations, 8 and 16 yr previously. In the 8‐yr experiment, SOC had declined under all rotations, with smaller changes where the rotation included 3 or 5 yr of perennial pasture. Whereas the average SOC was only 76% of the level in the preceding natural grassland, the corresponding value after 16 yr for the second site was 98% (and 93% under continuous arable), probably reflecting its high allophane clay content. The fractionation procedure tested proved applicable to both Andisols, but the intra‐aggregate light fraction (IA‐SOM, isolated in sodium iodide solution at 1.80 g/cm3 after ultrasonic dispersion) accounted for a very small proportion of total SOC (<1%). We suggest that in Andisols, the free light fraction (FR‐SOM, isolated in sodium iodide at solution of the same density, but prior to ultrasonic dispersion) is stabilised to a greater extent than in nonvolcanic soils, and the intra‐aggregate fraction plays a more minor role as a pool of intermediate turnover. The relative value of each fraction needs to be confirmed through dynamic experiments, using more sites, and including situations where SOC content is initially low.</abstract><cop>Oxford</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/sum.12070</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0266-0032 |
| ispartof | Soil use and management, 2013-12, Vol.29 (4), p.531-539 |
| issn | 0266-0032 1475-2743 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1475548813 |
| source | Wiley Online Library All Journals |
| subjects | Agronomy. Soil science and plant productions Andisols arable Arable land Biological and medical sciences Chemical, physicochemical, biochemical and biological properties Cropping systems. Cultivation. Soil tillage Density Dispersions Fractionation Fundamental and applied biological sciences. Psychology General agronomy. Plant production Generalities. Cropping systems and patterns Grasslands Indicators NaI Organic matter pasture physical fractionation Physics, chemistry, biochemistry and biology of agricultural and forest soils Soil (material) soil organic matter Soil science Volcanic soils |
| title | Free and intra-aggregate organic matter as indicators of soil quality change in volcanic soils under contrasting crop rotations |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T13%3A09%3A44IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Free%20and%20intra-aggregate%20organic%20matter%20as%20indicators%20of%20soil%20quality%20change%20in%20volcanic%20soils%20under%20contrasting%20crop%20rotations&rft.jtitle=Soil%20use%20and%20management&rft.au=Zagal,%20E.&rft.date=2013-12&rft.volume=29&rft.issue=4&rft.spage=531&rft.epage=539&rft.pages=531-539&rft.issn=0266-0032&rft.eissn=1475-2743&rft.coden=SUMAEU&rft_id=info:doi/10.1111/sum.12070&rft_dat=%3Cproquest_cross%3E3144553081%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1464541324&rft_id=info:pmid/&rfr_iscdi=true |