Mineralogical variations of bulk and rhizosphere soils from a Norway spruce stand

The mineralogy of bulk and rhizosphere soil materials was compared to assess the effect of roots on mineral weathering in a Podzol supporting a homogeneous Norway spruce [Picea abies (L.) Karst] stand. Six horizons were sampled in two profiles at the Skogaby site in southwestern Sweden. The soil adh...

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Veröffentlicht in:Soil Science Society of America journal 1997-07, Vol.61 (4), p.1245-1249
Hauptverfasser: Courchesne, F. (Universite de Montreal, Montreal, Canada.), Gobran, G.R
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creator Courchesne, F. (Universite de Montreal, Montreal, Canada.)
Gobran, G.R
description The mineralogy of bulk and rhizosphere soil materials was compared to assess the effect of roots on mineral weathering in a Podzol supporting a homogeneous Norway spruce [Picea abies (L.) Karst] stand. Six horizons were sampled in two profiles at the Skogaby site in southwestern Sweden. The soil adhering to the roots after shaking was considered as rhizosphere soil, a layer 3 mm thick intimately associated with root surfaces. The remaining material was regarded as bulk soil. The mineralogy of the clay-sized particles of both fractions was determined by x-ray diffraction (XRD) and normalized with respect to quartz (I/I(QZ)). Amorphous solid phases were estimated by extracting Fe and Al with acid-ammonium oxalate (Al0, Fe0). Mineral abundance (I/I(QZ)) near roots differed consistently from that in the bulk soil. The rhizosphere contained significantly lower amounts of amphiboles and expandable phyllosilicates (alpha
doi_str_mv 10.2136/sssaj1997.03615995006100040034x
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(Universite de Montreal, Montreal, Canada.)</creatorcontrib><creatorcontrib>Gobran, G.R</creatorcontrib><title>Mineralogical variations of bulk and rhizosphere soils from a Norway spruce stand</title><title>Soil Science Society of America journal</title><description>The mineralogy of bulk and rhizosphere soil materials was compared to assess the effect of roots on mineral weathering in a Podzol supporting a homogeneous Norway spruce [Picea abies (L.) Karst] stand. Six horizons were sampled in two profiles at the Skogaby site in southwestern Sweden. The soil adhering to the roots after shaking was considered as rhizosphere soil, a layer 3 mm thick intimately associated with root surfaces. The remaining material was regarded as bulk soil. The mineralogy of the clay-sized particles of both fractions was determined by x-ray diffraction (XRD) and normalized with respect to quartz (I/I(QZ)). Amorphous solid phases were estimated by extracting Fe and Al with acid-ammonium oxalate (Al0, Fe0). Mineral abundance (I/I(QZ)) near roots differed consistently from that in the bulk soil. The rhizosphere contained significantly lower amounts of amphiboles and expandable phyllosilicates (alpha</description><subject>Agronomy. Soil science and plant productions</subject><subject>ALTERATION ATMOSPHERIQUE</subject><subject>Biological and medical sciences</subject><subject>BULK SOILS VERSUS RHIZOSPHERE</subject><subject>CHARACTERIZATION</subject><subject>CONTENIDO MINERAL</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>METEORIZACION</subject><subject>MINERAL CONTENT</subject><subject>MINERALOGIA</subject><subject>MINERALOGIE</subject><subject>MINERALOGY</subject><subject>PICEA ABIES</subject><subject>PODZOL</subject><subject>PODZOLES</subject><subject>PODZOLS</subject><subject>RHIZOSPHERE</subject><subject>RIZOSFERA</subject><subject>Silicates</subject><subject>SOIL</subject><subject>Soil genesis</subject><subject>Soil science</subject><subject>Soil surveys, classification and mapping, soil genesis</subject><subject>Soils</subject><subject>SOL</subject><subject>SOL DE FORET</subject><subject>SUECIA</subject><subject>SUEDE</subject><subject>SUELO</subject><subject>SUELO FORESTAL</subject><subject>Surficial geology</subject><subject>SWEDEN</subject><subject>TENEUR EN ELEMENTS MINERAUX</subject><subject>WEATHERING</subject><issn>0361-5995</issn><issn>1435-0661</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNqVkE1vEzEQhi0EEqHwE5B8QHDaMrP-2PUJVRWfaotQqNSbNbvxti6bdfAklPDrcZqqp156sSX78fuOHyHeIRzWqOx7ZqZrdK45BGXROGcALAKABlD67xMxQ61MBdbiUzHbMdUOei5eMF8DlBcAM_HjNE4h05guY0-j_EM50jqmiWUaZLcZf0maFjJfxX-JV1chB8kpjiyHnJaS5FnKN7SVvMqbvlytC_xSPBto5PDqbj8Q558-_jz-Up18__z1-OikIm31RWWwCXahGmscdo3uggK0g6MWF2gN9EGXEwIwDVldY0ttpztTD70jtyi_Vgfi7T53ldPvTeC1X0buwzjSFNKGPVqsVa1UAT_swT4n5hwGv8pxSXnrEfxOpb9X6R9UWRLe3FURF0tDpqmPfB9Tt8a0Dgvm99hNHMP2sS1-fvStns_LumMeQi5Kw-t9w0DJ02UuQ5zPb_GiUzXqP5kJmQ4</recordid><startdate>199707</startdate><enddate>199707</enddate><creator>Courchesne, F. 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Soil science and plant productions</topic><topic>ALTERATION ATMOSPHERIQUE</topic><topic>Biological and medical sciences</topic><topic>BULK SOILS VERSUS RHIZOSPHERE</topic><topic>CHARACTERIZATION</topic><topic>CONTENIDO MINERAL</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>METEORIZACION</topic><topic>MINERAL CONTENT</topic><topic>MINERALOGIA</topic><topic>MINERALOGIE</topic><topic>MINERALOGY</topic><topic>PICEA ABIES</topic><topic>PODZOL</topic><topic>PODZOLES</topic><topic>PODZOLS</topic><topic>RHIZOSPHERE</topic><topic>RIZOSFERA</topic><topic>Silicates</topic><topic>SOIL</topic><topic>Soil genesis</topic><topic>Soil science</topic><topic>Soil surveys, classification and mapping, soil genesis</topic><topic>Soils</topic><topic>SOL</topic><topic>SOL DE FORET</topic><topic>SUECIA</topic><topic>SUEDE</topic><topic>SUELO</topic><topic>SUELO FORESTAL</topic><topic>Surficial geology</topic><topic>SWEDEN</topic><topic>TENEUR EN ELEMENTS MINERAUX</topic><topic>WEATHERING</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Courchesne, F. (Universite de Montreal, Montreal, Canada.)</creatorcontrib><creatorcontrib>Gobran, G.R</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Biotechnology Research Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>Soil Science Society of America journal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Courchesne, F. (Universite de Montreal, Montreal, Canada.)</au><au>Gobran, G.R</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mineralogical variations of bulk and rhizosphere soils from a Norway spruce stand</atitle><jtitle>Soil Science Society of America journal</jtitle><date>1997-07</date><risdate>1997</risdate><volume>61</volume><issue>4</issue><spage>1245</spage><epage>1249</epage><pages>1245-1249</pages><issn>0361-5995</issn><eissn>1435-0661</eissn><coden>SSSJD4</coden><abstract>The mineralogy of bulk and rhizosphere soil materials was compared to assess the effect of roots on mineral weathering in a Podzol supporting a homogeneous Norway spruce [Picea abies (L.) Karst] stand. Six horizons were sampled in two profiles at the Skogaby site in southwestern Sweden. The soil adhering to the roots after shaking was considered as rhizosphere soil, a layer 3 mm thick intimately associated with root surfaces. The remaining material was regarded as bulk soil. The mineralogy of the clay-sized particles of both fractions was determined by x-ray diffraction (XRD) and normalized with respect to quartz (I/I(QZ)). Amorphous solid phases were estimated by extracting Fe and Al with acid-ammonium oxalate (Al0, Fe0). Mineral abundance (I/I(QZ)) near roots differed consistently from that in the bulk soil. The rhizosphere contained significantly lower amounts of amphiboles and expandable phyllosilicates (alpha</abstract><cop>Madison, WI</cop><pub>Soil Science Society of America</pub><doi>10.2136/sssaj1997.03615995006100040034x</doi><tpages>5</tpages></addata></record>
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source Wiley Online Library Journals Frontfile Complete
subjects Agronomy. Soil science and plant productions
ALTERATION ATMOSPHERIQUE
Biological and medical sciences
BULK SOILS VERSUS RHIZOSPHERE
CHARACTERIZATION
CONTENIDO MINERAL
Earth sciences
Earth, ocean, space
Exact sciences and technology
FOREST SOILS
Fundamental and applied biological sciences. Psychology
METEORIZACION
MINERAL CONTENT
MINERALOGIA
MINERALOGIE
MINERALOGY
PICEA ABIES
PODZOL
PODZOLES
PODZOLS
RHIZOSPHERE
RIZOSFERA
Silicates
SOIL
Soil genesis
Soil science
Soil surveys, classification and mapping, soil genesis
Soils
SOL
SOL DE FORET
SUECIA
SUEDE
SUELO
SUELO FORESTAL
Surficial geology
SWEDEN
TENEUR EN ELEMENTS MINERAUX
WEATHERING
title Mineralogical variations of bulk and rhizosphere soils from a Norway spruce stand
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