Root impact on the stability and types of micro-aggregates in silty soil under maize

Summary We wished to assess the impact of maize roots on the stability, nature and formation of soil organomineral aggregates under field conditions. We sampled coarse‐textured soil, cropped with maize for 3 years, and combined in situ study of the root system with evaluation of soil structural stab...

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Veröffentlicht in:European journal of soil science 2006-04, Vol.57 (2), p.247-257
Hauptverfasser: Watteau, F., Villemin, G., Burtin, G., Jocteur-Monrozier, L.
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Burtin, G.
Jocteur-Monrozier, L.
description Summary We wished to assess the impact of maize roots on the stability, nature and formation of soil organomineral aggregates under field conditions. We sampled coarse‐textured soil, cropped with maize for 3 years, and combined in situ study of the root system with evaluation of soil structural stability. We examined root morphology (i) on thin sections of still recognizable root tissues, and (ii) at the interfaces between roots and soil, using transmission electron microscopy (TEM) to differentiate between fine and coarse roots. Soil structural stability was evaluated in relation to a spatial gradient of increasing distance from the roots. For that we distinguished between soil adhering to roots and that not adhering in the rhizosphere, and soil between the rows of this crop, and used two methods of granulodensimetric soil fractionation involving different disaggregation strengths. We isolated and identified the organomineral associations in the soil fractions determining soil stability. We found that the roots at the soil–root interface generated stable aggregates of 2–20 µm size, which were much involved in the structural stability of the soil adhering to roots. We identified by TEM several types of organomineral associations that depended on the nature of the plant or microbial organic matter. The distribution of the different types of aggregates varied according to their positions in relation to the roots. We showed that humification of roots contributes significantly to the development of stable organomineral associations in the soil. L'influence des racines de maïs sur la stabilité et la nature des microagregats d'un sol limoneux Résumé L'objectif de cette étude est de suivre au champ, l'influence des racines de maïs sur la stabilité des associations organo‐minérales, leur nature et leur formation. Pour cela, nous avons échantillonné au sein d'un sol à texture grossière, cultivé depuis trois ans en maïs, et associé deux approches: une étude in situ du système racinaire du maïs et une évaluation de la stabilité structurale du sol. L'étude du système racinaire comporte en particulier une description morphologique (i) des tissus racinaires observables à l'échelle de la lame mince et (ii) des interfaces racines–sol à l'échelle ultrastructurale en microscopie électronique à transmission (MET), en distinguant les racines fines et les racines adventives. L'évaluation de la stabilité structurale du sol est réalisée selon un gradient spatial d'éloignement pa
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We sampled coarse‐textured soil, cropped with maize for 3 years, and combined in situ study of the root system with evaluation of soil structural stability. We examined root morphology (i) on thin sections of still recognizable root tissues, and (ii) at the interfaces between roots and soil, using transmission electron microscopy (TEM) to differentiate between fine and coarse roots. Soil structural stability was evaluated in relation to a spatial gradient of increasing distance from the roots. For that we distinguished between soil adhering to roots and that not adhering in the rhizosphere, and soil between the rows of this crop, and used two methods of granulodensimetric soil fractionation involving different disaggregation strengths. We isolated and identified the organomineral associations in the soil fractions determining soil stability. We found that the roots at the soil–root interface generated stable aggregates of 2–20 µm size, which were much involved in the structural stability of the soil adhering to roots. We identified by TEM several types of organomineral associations that depended on the nature of the plant or microbial organic matter. The distribution of the different types of aggregates varied according to their positions in relation to the roots. We showed that humification of roots contributes significantly to the development of stable organomineral associations in the soil. L'influence des racines de maïs sur la stabilité et la nature des microagregats d'un sol limoneux Résumé L'objectif de cette étude est de suivre au champ, l'influence des racines de maïs sur la stabilité des associations organo‐minérales, leur nature et leur formation. Pour cela, nous avons échantillonné au sein d'un sol à texture grossière, cultivé depuis trois ans en maïs, et associé deux approches: une étude in situ du système racinaire du maïs et une évaluation de la stabilité structurale du sol. L'étude du système racinaire comporte en particulier une description morphologique (i) des tissus racinaires observables à l'échelle de la lame mince et (ii) des interfaces racines–sol à l'échelle ultrastructurale en microscopie électronique à transmission (MET), en distinguant les racines fines et les racines adventives. L'évaluation de la stabilité structurale du sol est réalisée selon un gradient spatial d'éloignement par rapport aux racines, en distinguant le sol rhizosphérique adhérent aux racines, le sol rhizosphérique non adhérent et le sol sans plante prélevé dans les inter‐rangs. Cette évaluation est basée sur l'utilisation de deux fractionnements granulo‐densimétriques du sol, mettant en œuvre des forces de dispersion différentes. Les résultats montrent la capacité des racines à générer des microagrégats (2–20 µm) au niveau des interfaces sol–racines, ces associations organo‐minérales se révélant fortement impliquées dans la stabilité structurale du sol adhérent. Plusieurs types de microagrégats ont été déterminés en MET, en fonction de la nature des matières organiques végétales ou microbiennes impliquées, et leur distribution est différente selon leur localisation par rapport aux racines. Les résultats mettent en évidence la contribution de l'humification racinaire dans l'évolution des associations organo‐minérales stables de ce sol.</description><identifier>ISSN: 1351-0754</identifier><identifier>EISSN: 1365-2389</identifier><identifier>DOI: 10.1111/j.1365-2389.2005.00734.x</identifier><language>eng</language><publisher>Oxford, UK; Malden, USA: Blackwell Science Ltd</publisher><subject>Agronomy. Soil science and plant productions ; Biological and medical sciences ; Chemical, physicochemical, biochemical and biological properties ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Organic matter ; Physical properties ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Soil science ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Structure, texture, density, mechanical behavior. 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We sampled coarse‐textured soil, cropped with maize for 3 years, and combined in situ study of the root system with evaluation of soil structural stability. We examined root morphology (i) on thin sections of still recognizable root tissues, and (ii) at the interfaces between roots and soil, using transmission electron microscopy (TEM) to differentiate between fine and coarse roots. Soil structural stability was evaluated in relation to a spatial gradient of increasing distance from the roots. For that we distinguished between soil adhering to roots and that not adhering in the rhizosphere, and soil between the rows of this crop, and used two methods of granulodensimetric soil fractionation involving different disaggregation strengths. We isolated and identified the organomineral associations in the soil fractions determining soil stability. We found that the roots at the soil–root interface generated stable aggregates of 2–20 µm size, which were much involved in the structural stability of the soil adhering to roots. We identified by TEM several types of organomineral associations that depended on the nature of the plant or microbial organic matter. The distribution of the different types of aggregates varied according to their positions in relation to the roots. We showed that humification of roots contributes significantly to the development of stable organomineral associations in the soil. L'influence des racines de maïs sur la stabilité et la nature des microagregats d'un sol limoneux Résumé L'objectif de cette étude est de suivre au champ, l'influence des racines de maïs sur la stabilité des associations organo‐minérales, leur nature et leur formation. Pour cela, nous avons échantillonné au sein d'un sol à texture grossière, cultivé depuis trois ans en maïs, et associé deux approches: une étude in situ du système racinaire du maïs et une évaluation de la stabilité structurale du sol. L'étude du système racinaire comporte en particulier une description morphologique (i) des tissus racinaires observables à l'échelle de la lame mince et (ii) des interfaces racines–sol à l'échelle ultrastructurale en microscopie électronique à transmission (MET), en distinguant les racines fines et les racines adventives. L'évaluation de la stabilité structurale du sol est réalisée selon un gradient spatial d'éloignement par rapport aux racines, en distinguant le sol rhizosphérique adhérent aux racines, le sol rhizosphérique non adhérent et le sol sans plante prélevé dans les inter‐rangs. Cette évaluation est basée sur l'utilisation de deux fractionnements granulo‐densimétriques du sol, mettant en œuvre des forces de dispersion différentes. Les résultats montrent la capacité des racines à générer des microagrégats (2–20 µm) au niveau des interfaces sol–racines, ces associations organo‐minérales se révélant fortement impliquées dans la stabilité structurale du sol adhérent. Plusieurs types de microagrégats ont été déterminés en MET, en fonction de la nature des matières organiques végétales ou microbiennes impliquées, et leur distribution est différente selon leur localisation par rapport aux racines. Les résultats mettent en évidence la contribution de l'humification racinaire dans l'évolution des associations organo‐minérales stables de ce sol.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Organic matter</subject><subject>Physical properties</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Soil science</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. Amendments</subject><subject>Structure, texture, density, mechanical behavior. Heat and gas exchanges</subject><subject>Zea mays</subject><issn>1351-0754</issn><issn>1365-2389</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqNkEtPGzEURkdVkaDAf_Cm3c3Ur3l40UUVUcpDIAUIKBvL47lOnc4j2I5I-PV4CIIt3vjK9zvXuidJEMEZiefnMiOsyFPKKpFRjPMM45LxbPMlOXhvfB3rnKS4zPl-8s37JcaEESEOktvpMARku5XSAQ09Cv8A-aBq29qwRapvUNiuwKPBoM5qN6RqsXCwUCG-2R5528aYH2yL1n0DDnXKPsNRsmdU6-H47T5M7v6c3E7-ppfXp2eT35ep5oTyVBhcc2EEABNU1MyouqFVQcpaA-EVEybnuqorqjUUpiiaQmsKNVdMYFY3mB0mP3ZzV254XIMPsrNeQ9uqHoa1l0RUnJWUxWC1C8YNvHdg5MrZTrmtJFiOGuVSjrbkaEuOGuWrRrmJ6Pe3P5TXqjVO9dr6D74sMKtyHnO_drkn28L20_PlyfnNTawin-546wNs3nnl_suiZGUu769O5XQ2m19Q8iDn7AXfUZYU</recordid><startdate>200604</startdate><enddate>200604</enddate><creator>Watteau, F.</creator><creator>Villemin, G.</creator><creator>Burtin, G.</creator><creator>Jocteur-Monrozier, L.</creator><general>Blackwell Science Ltd</general><general>Blackwell Science</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7T7</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>P64</scope></search><sort><creationdate>200604</creationdate><title>Root impact on the stability and types of micro-aggregates in silty soil under maize</title><author>Watteau, F. ; Villemin, G. ; Burtin, G. ; Jocteur-Monrozier, L.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4124-9f0b49f9ee3929b3fabd28617bce14839f54c8b82cce6f66d6cc2eb4a3903bd03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>Organic matter</topic><topic>Physical properties</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Soil science</topic><topic>Soil-plant relationships. Soil fertility</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>Structure, texture, density, mechanical behavior. Heat and gas exchanges</topic><topic>Zea mays</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Watteau, F.</creatorcontrib><creatorcontrib>Villemin, G.</creatorcontrib><creatorcontrib>Burtin, G.</creatorcontrib><creatorcontrib>Jocteur-Monrozier, L.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>European journal of soil science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Watteau, F.</au><au>Villemin, G.</au><au>Burtin, G.</au><au>Jocteur-Monrozier, L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Root impact on the stability and types of micro-aggregates in silty soil under maize</atitle><jtitle>European journal of soil science</jtitle><date>2006-04</date><risdate>2006</risdate><volume>57</volume><issue>2</issue><spage>247</spage><epage>257</epage><pages>247-257</pages><issn>1351-0754</issn><eissn>1365-2389</eissn><abstract>Summary We wished to assess the impact of maize roots on the stability, nature and formation of soil organomineral aggregates under field conditions. We sampled coarse‐textured soil, cropped with maize for 3 years, and combined in situ study of the root system with evaluation of soil structural stability. We examined root morphology (i) on thin sections of still recognizable root tissues, and (ii) at the interfaces between roots and soil, using transmission electron microscopy (TEM) to differentiate between fine and coarse roots. Soil structural stability was evaluated in relation to a spatial gradient of increasing distance from the roots. For that we distinguished between soil adhering to roots and that not adhering in the rhizosphere, and soil between the rows of this crop, and used two methods of granulodensimetric soil fractionation involving different disaggregation strengths. We isolated and identified the organomineral associations in the soil fractions determining soil stability. We found that the roots at the soil–root interface generated stable aggregates of 2–20 µm size, which were much involved in the structural stability of the soil adhering to roots. We identified by TEM several types of organomineral associations that depended on the nature of the plant or microbial organic matter. The distribution of the different types of aggregates varied according to their positions in relation to the roots. We showed that humification of roots contributes significantly to the development of stable organomineral associations in the soil. L'influence des racines de maïs sur la stabilité et la nature des microagregats d'un sol limoneux Résumé L'objectif de cette étude est de suivre au champ, l'influence des racines de maïs sur la stabilité des associations organo‐minérales, leur nature et leur formation. Pour cela, nous avons échantillonné au sein d'un sol à texture grossière, cultivé depuis trois ans en maïs, et associé deux approches: une étude in situ du système racinaire du maïs et une évaluation de la stabilité structurale du sol. L'étude du système racinaire comporte en particulier une description morphologique (i) des tissus racinaires observables à l'échelle de la lame mince et (ii) des interfaces racines–sol à l'échelle ultrastructurale en microscopie électronique à transmission (MET), en distinguant les racines fines et les racines adventives. L'évaluation de la stabilité structurale du sol est réalisée selon un gradient spatial d'éloignement par rapport aux racines, en distinguant le sol rhizosphérique adhérent aux racines, le sol rhizosphérique non adhérent et le sol sans plante prélevé dans les inter‐rangs. Cette évaluation est basée sur l'utilisation de deux fractionnements granulo‐densimétriques du sol, mettant en œuvre des forces de dispersion différentes. Les résultats montrent la capacité des racines à générer des microagrégats (2–20 µm) au niveau des interfaces sol–racines, ces associations organo‐minérales se révélant fortement impliquées dans la stabilité structurale du sol adhérent. Plusieurs types de microagrégats ont été déterminés en MET, en fonction de la nature des matières organiques végétales ou microbiennes impliquées, et leur distribution est différente selon leur localisation par rapport aux racines. Les résultats mettent en évidence la contribution de l'humification racinaire dans l'évolution des associations organo‐minérales stables de ce sol.</abstract><cop>Oxford, UK; Malden, USA</cop><pub>Blackwell Science Ltd</pub><doi>10.1111/j.1365-2389.2005.00734.x</doi><tpages>11</tpages></addata></record>
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subjects Agronomy. Soil science and plant productions
Biological and medical sciences
Chemical, physicochemical, biochemical and biological properties
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Organic matter
Physical properties
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Soil science
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Structure, texture, density, mechanical behavior. Heat and gas exchanges
Zea mays
title Root impact on the stability and types of micro-aggregates in silty soil under maize
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