Soil aggregate stability in Mediterranean and tropical agro-ecosystems: effect of plant roots and soil characteristics
Aims Our aim was to determine the effect of soil characteristics and root traits on soil aggregate stability at an inter- and intra-site scale in a range of agro-ecosystems. We also evaluated the effect of soil depth and the type of land use on aggregate stability. Methods Soil aggregate stability,...
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| Veröffentlicht in: | Plant and soil 2018-03, Vol.424 (1/2), p.303-317 |
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| creator | Le Bissonnais, Yves Prieto, Iván Roumet, Catherine Nespoulous, Jérôme Metayer, James Huon, Sylvain Villatoro, Mario Stokes, Alexia |
| description | Aims Our aim was to determine the effect of soil characteristics and root traits on soil aggregate stability at an inter- and intra-site scale in a range of agro-ecosystems. We also evaluated the effect of soil depth and the type of land use on aggregate stability. Methods Soil aggregate stability, soil physicochemical properties and fine root traits were measured along land use gradients (from monocultures to agroforestry systems and forests), at two soil depths at four sites (Mediterranean and tropical climates) with contrasting soils (Andosol, Ferralsol, Leptosol and Fluvisol). Results Aggregate stability was much lower in deep than in surface soil layers, likely linked to lower soil organic carbon (SOC) and lower root mass density (RMD). Locally, and consistently in all sites, land use intensification degrades soil aggregate stability, mainly in surface soil layers. Soil organic carbon, cation exchange capacity and root traits: water-soluble compounds, lignin and medium root length proportion were the most important drivers of aggregate stability at the inter-site level, whereas SOC, root mass and root length densities (RMD, RLD) were the main drivers at the intra-site level. Conclusions Overall, the data suggest different controls on soil aggregate stability globally (soil) and locally (roots). Conversion from forests to agricultural land will likely lead to greater C losses through a loss of aggregate stability and increased soil erosion. |
| doi_str_mv | 10.1007/s11104-017-3423-6 |
| format | Article |
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We also evaluated the effect of soil depth and the type of land use on aggregate stability. Methods Soil aggregate stability, soil physicochemical properties and fine root traits were measured along land use gradients (from monocultures to agroforestry systems and forests), at two soil depths at four sites (Mediterranean and tropical climates) with contrasting soils (Andosol, Ferralsol, Leptosol and Fluvisol). Results Aggregate stability was much lower in deep than in surface soil layers, likely linked to lower soil organic carbon (SOC) and lower root mass density (RMD). Locally, and consistently in all sites, land use intensification degrades soil aggregate stability, mainly in surface soil layers. Soil organic carbon, cation exchange capacity and root traits: water-soluble compounds, lignin and medium root length proportion were the most important drivers of aggregate stability at the inter-site level, whereas SOC, root mass and root length densities (RMD, RLD) were the main drivers at the intra-site level. Conclusions Overall, the data suggest different controls on soil aggregate stability globally (soil) and locally (roots). Conversion from forests to agricultural land will likely lead to greater C losses through a loss of aggregate stability and increased soil erosion.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-017-3423-6</identifier><language>eng</language><publisher>Cham: Springer</publisher><subject>Agricultural ecosystems ; Agricultural land ; Agroforestry ; Biomedical and Life Sciences ; Cation exchange ; Cation exchanging ; Control stability ; Ecology ; Ecosystem assessment ; Erosion ; Forests ; Land use ; Life Sciences ; Lignin ; Monoculture ; Observations ; Organic carbon ; Organic soils ; Physicochemical properties ; Plant Physiology ; Plant roots ; Plant Sciences ; Plant-soil relationships ; Rain ; Regular Article ; Roots ; Soil aggregates ; Soil characteristics ; Soil degradation ; Soil depth ; Soil erosion ; Soil infiltration ; Soil layers ; Soil properties ; Soil Science & Conservation ; Soil stability ; Soil surfaces ; Surface stability</subject><ispartof>Plant and soil, 2018-03, Vol.424 (1/2), p.303-317</ispartof><rights>Springer International Publishing AG, part of Springer Nature 2018</rights><rights>Springer International Publishing AG 2017</rights><rights>COPYRIGHT 2018 Springer</rights><rights>Plant and Soil is a copyright of Springer, (2017). All Rights Reserved.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c411t-8e5d8f8b89af6540161dc4d31b87cdda4e116028c4303ec6e617689702e933e73</citedby><cites>FETCH-LOGICAL-c411t-8e5d8f8b89af6540161dc4d31b87cdda4e116028c4303ec6e617689702e933e73</cites><orcidid>0000-0001-5549-1132 ; 0000-0002-2276-0911 ; 0000-0003-1320-9770 ; 0000-0001-5325-7174 ; 0000-0003-3013-2605</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26652037$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26652037$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,776,780,799,881,27901,27902,41464,42533,51294,57992,58225</link.rule.ids><backlink>$$Uhttps://hal.science/hal-01837402$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Le Bissonnais, Yves</creatorcontrib><creatorcontrib>Prieto, Iván</creatorcontrib><creatorcontrib>Roumet, Catherine</creatorcontrib><creatorcontrib>Nespoulous, Jérôme</creatorcontrib><creatorcontrib>Metayer, James</creatorcontrib><creatorcontrib>Huon, Sylvain</creatorcontrib><creatorcontrib>Villatoro, Mario</creatorcontrib><creatorcontrib>Stokes, Alexia</creatorcontrib><title>Soil aggregate stability in Mediterranean and tropical agro-ecosystems: effect of plant roots and soil characteristics</title><title>Plant and soil</title><addtitle>Plant Soil</addtitle><description>Aims Our aim was to determine the effect of soil characteristics and root traits on soil aggregate stability at an inter- and intra-site scale in a range of agro-ecosystems. We also evaluated the effect of soil depth and the type of land use on aggregate stability. Methods Soil aggregate stability, soil physicochemical properties and fine root traits were measured along land use gradients (from monocultures to agroforestry systems and forests), at two soil depths at four sites (Mediterranean and tropical climates) with contrasting soils (Andosol, Ferralsol, Leptosol and Fluvisol). Results Aggregate stability was much lower in deep than in surface soil layers, likely linked to lower soil organic carbon (SOC) and lower root mass density (RMD). Locally, and consistently in all sites, land use intensification degrades soil aggregate stability, mainly in surface soil layers. Soil organic carbon, cation exchange capacity and root traits: water-soluble compounds, lignin and medium root length proportion were the most important drivers of aggregate stability at the inter-site level, whereas SOC, root mass and root length densities (RMD, RLD) were the main drivers at the intra-site level. Conclusions Overall, the data suggest different controls on soil aggregate stability globally (soil) and locally (roots). Conversion from forests to agricultural land will likely lead to greater C losses through a loss of aggregate stability and increased soil erosion.</description><subject>Agricultural ecosystems</subject><subject>Agricultural land</subject><subject>Agroforestry</subject><subject>Biomedical and Life Sciences</subject><subject>Cation exchange</subject><subject>Cation exchanging</subject><subject>Control stability</subject><subject>Ecology</subject><subject>Ecosystem assessment</subject><subject>Erosion</subject><subject>Forests</subject><subject>Land use</subject><subject>Life Sciences</subject><subject>Lignin</subject><subject>Monoculture</subject><subject>Observations</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Physicochemical properties</subject><subject>Plant Physiology</subject><subject>Plant roots</subject><subject>Plant Sciences</subject><subject>Plant-soil relationships</subject><subject>Rain</subject><subject>Regular Article</subject><subject>Roots</subject><subject>Soil aggregates</subject><subject>Soil characteristics</subject><subject>Soil degradation</subject><subject>Soil depth</subject><subject>Soil erosion</subject><subject>Soil infiltration</subject><subject>Soil layers</subject><subject>Soil properties</subject><subject>Soil Science & Conservation</subject><subject>Soil stability</subject><subject>Soil surfaces</subject><subject>Surface stability</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kUGLFDEQhYMoOK7-AA9CwJOHXquSdNLtbVhWd2HEgwreQiZd3ZuhpzMm2YX593bbst6WHEKK99V74TH2FuESAczHjIigKkBTSSVkpZ-xDdZGVjVI_ZxtAKSowLS_XrJXOR9geaPesIfvMYzcDUOiwRXiubh9GEM58zDxr9SFQim5idzE3dTxkuIpeLcQKVbkYz7nQsf8iVPfky889vw0uqnwFGPJf5m8OPg7l5yfl4Vcgs-v2YvejZne_Lsv2M_P1z-ubqrdty-3V9td5RViqRqqu6Zv9k3rel0rQI2dV53EfWN81zlFiBpE45UESV6TRqOb1oCgVkoy8oJ9WPfeudGeUji6dLbRBXuz3dllBthIo0A84Kx9v2pPKf6-p1zsId6naY5nBYha11K2elZdrqrBjWTD1Mcyf2w-HR2DjxP1YZ5va6naxgi1RMAV8CnmnKh_zIFgl-7s2t0cxdilO7uYiJXJs3YaKP2P8hT0boUOucT06CK0rgVII_8AmaKleA</recordid><startdate>20180301</startdate><enddate>20180301</enddate><creator>Le Bissonnais, Yves</creator><creator>Prieto, Iván</creator><creator>Roumet, Catherine</creator><creator>Nespoulous, Jérôme</creator><creator>Metayer, James</creator><creator>Huon, Sylvain</creator><creator>Villatoro, Mario</creator><creator>Stokes, Alexia</creator><general>Springer</general><general>Springer International Publishing</general><general>Springer Nature B.V</general><general>Springer Verlag</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>88A</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>P64</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>SOI</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0001-5549-1132</orcidid><orcidid>https://orcid.org/0000-0002-2276-0911</orcidid><orcidid>https://orcid.org/0000-0003-1320-9770</orcidid><orcidid>https://orcid.org/0000-0001-5325-7174</orcidid><orcidid>https://orcid.org/0000-0003-3013-2605</orcidid></search><sort><creationdate>20180301</creationdate><title>Soil aggregate stability in Mediterranean and tropical agro-ecosystems: effect of plant roots and soil characteristics</title><author>Le Bissonnais, Yves ; 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We also evaluated the effect of soil depth and the type of land use on aggregate stability. Methods Soil aggregate stability, soil physicochemical properties and fine root traits were measured along land use gradients (from monocultures to agroforestry systems and forests), at two soil depths at four sites (Mediterranean and tropical climates) with contrasting soils (Andosol, Ferralsol, Leptosol and Fluvisol). Results Aggregate stability was much lower in deep than in surface soil layers, likely linked to lower soil organic carbon (SOC) and lower root mass density (RMD). Locally, and consistently in all sites, land use intensification degrades soil aggregate stability, mainly in surface soil layers. Soil organic carbon, cation exchange capacity and root traits: water-soluble compounds, lignin and medium root length proportion were the most important drivers of aggregate stability at the inter-site level, whereas SOC, root mass and root length densities (RMD, RLD) were the main drivers at the intra-site level. Conclusions Overall, the data suggest different controls on soil aggregate stability globally (soil) and locally (roots). Conversion from forests to agricultural land will likely lead to greater C losses through a loss of aggregate stability and increased soil erosion.</abstract><cop>Cham</cop><pub>Springer</pub><doi>10.1007/s11104-017-3423-6</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0001-5549-1132</orcidid><orcidid>https://orcid.org/0000-0002-2276-0911</orcidid><orcidid>https://orcid.org/0000-0003-1320-9770</orcidid><orcidid>https://orcid.org/0000-0001-5325-7174</orcidid><orcidid>https://orcid.org/0000-0003-3013-2605</orcidid></addata></record> |
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| subjects | Agricultural ecosystems Agricultural land Agroforestry Biomedical and Life Sciences Cation exchange Cation exchanging Control stability Ecology Ecosystem assessment Erosion Forests Land use Life Sciences Lignin Monoculture Observations Organic carbon Organic soils Physicochemical properties Plant Physiology Plant roots Plant Sciences Plant-soil relationships Rain Regular Article Roots Soil aggregates Soil characteristics Soil degradation Soil depth Soil erosion Soil infiltration Soil layers Soil properties Soil Science & Conservation Soil stability Soil surfaces Surface stability |
| title | Soil aggregate stability in Mediterranean and tropical agro-ecosystems: effect of plant roots and soil characteristics |
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