Illite transformation and potassium release upon changes in composition of the rhizophere soil solution
Aims and background Release of 'non-exchangeable' potassium (K) from interlayers of illite is diffusioncontrolled and has been shown to depend on the solution concentration of Ê and other cations (Ca²⁺, Mg²⁺, NH₄⁺). Methods We analysed changes in soil solution concentrations of K and compe...
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| Veröffentlicht in: | Plant and soil 2013-10, Vol.371 (1/2), p.267-279 |
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| creator | Vetterlein, Doris Kühn, Thomas Kaiser, Klaus Jahn, Reinhold |
| description | Aims and background Release of 'non-exchangeable' potassium (K) from interlayers of illite is diffusioncontrolled and has been shown to depend on the solution concentration of Ê and other cations (Ca²⁺, Mg²⁺, NH₄⁺). Methods We analysed changes in soil solution concentrations of K and competing cations in situ at different distances from the root surface over time and related them to the transformation of illite, as revealed by X-ray diffraction, and chemical measures of differently bound K. Results and Conclusions Within 49 and 98 days, respectively, 6.4 and 14.4 % of the illite's total K was released upon contact with the root system. Mixed layered minerals increased from 33 (0 d) to 35 (49 d) to 40 % (98 d). Release of K from interlayers and the transformation of illite occurred at soil solution K concentrations close to the threshold of 80 µM suggested earlier. Concentrations of Ca and Mg increased with decreasing distance from the root surface, promoting the release of K. The NaBPh₄ method supposed to determine 'non-exchangeable' K extracted only 1/3 of the total K from illite. |
| doi_str_mv | 10.1007/s11104-013-1680-6 |
| format | Article |
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Methods We analysed changes in soil solution concentrations of K and competing cations in situ at different distances from the root surface over time and related them to the transformation of illite, as revealed by X-ray diffraction, and chemical measures of differently bound K. Results and Conclusions Within 49 and 98 days, respectively, 6.4 and 14.4 % of the illite's total K was released upon contact with the root system. Mixed layered minerals increased from 33 (0 d) to 35 (49 d) to 40 % (98 d). Release of K from interlayers and the transformation of illite occurred at soil solution K concentrations close to the threshold of 80 µM suggested earlier. Concentrations of Ca and Mg increased with decreasing distance from the root surface, promoting the release of K. The NaBPh₄ method supposed to determine 'non-exchangeable' K extracted only 1/3 of the total K from illite.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-013-1680-6</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Agricultural soils ; Agronomy. Soil science and plant productions ; Animal, plant and microbial ecology ; Biogeochemistry ; Biological and medical sciences ; Biomedical and Life Sciences ; Cations ; Chemical properties ; Clay soils ; Ecology ; Environmental aspects ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Identification and classification ; Illite ; Life Sciences ; Minerals ; Physical properties ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Plant Physiology ; Plant roots ; Plant Sciences ; Plants ; Potassium ; Regular Article ; Rhizosphere ; Soil chemistry ; Soil composition ; Soil conditioners ; Soil microorganisms ; Soil science ; Soil Science & Conservation ; Soil solution ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Vermiculite ; Water and solute dynamics ; X-ray diffraction</subject><ispartof>Plant and soil, 2013-10, Vol.371 (1/2), p.267-279</ispartof><rights>2013 Springer</rights><rights>Springer Science+Business Media Dordrecht 2013</rights><rights>2014 INIST-CNRS</rights><rights>COPYRIGHT 2013 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c440t-5a3b6c68325b3866f23ab7e0fc0e48c4ee9186c4df3dc04230484a42419cdefe3</citedby><cites>FETCH-LOGICAL-c440t-5a3b6c68325b3866f23ab7e0fc0e48c4ee9186c4df3dc04230484a42419cdefe3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42952719$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42952719$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>315,781,785,804,27928,27929,41492,42561,51323,58021,58254</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27774550$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Vetterlein, Doris</creatorcontrib><creatorcontrib>Kühn, Thomas</creatorcontrib><creatorcontrib>Kaiser, Klaus</creatorcontrib><creatorcontrib>Jahn, Reinhold</creatorcontrib><title>Illite transformation and potassium release upon changes in composition of the rhizophere soil solution</title><title>Plant and soil</title><addtitle>Plant Soil</addtitle><description>Aims and background Release of 'non-exchangeable' potassium (K) from interlayers of illite is diffusioncontrolled and has been shown to depend on the solution concentration of Ê and other cations (Ca²⁺, Mg²⁺, NH₄⁺). Methods We analysed changes in soil solution concentrations of K and competing cations in situ at different distances from the root surface over time and related them to the transformation of illite, as revealed by X-ray diffraction, and chemical measures of differently bound K. Results and Conclusions Within 49 and 98 days, respectively, 6.4 and 14.4 % of the illite's total K was released upon contact with the root system. Mixed layered minerals increased from 33 (0 d) to 35 (49 d) to 40 % (98 d). Release of K from interlayers and the transformation of illite occurred at soil solution K concentrations close to the threshold of 80 µM suggested earlier. Concentrations of Ca and Mg increased with decreasing distance from the root surface, promoting the release of K. The NaBPh₄ method supposed to determine 'non-exchangeable' K extracted only 1/3 of the total K from illite.</description><subject>Agricultural soils</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Animal, plant and microbial ecology</subject><subject>Biogeochemistry</subject><subject>Biological and medical sciences</subject><subject>Biomedical and Life Sciences</subject><subject>Cations</subject><subject>Chemical properties</subject><subject>Clay soils</subject><subject>Ecology</subject><subject>Environmental aspects</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Identification and classification</subject><subject>Illite</subject><subject>Life Sciences</subject><subject>Minerals</subject><subject>Physical properties</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Plant Physiology</subject><subject>Plant roots</subject><subject>Plant Sciences</subject><subject>Plants</subject><subject>Potassium</subject><subject>Regular Article</subject><subject>Rhizosphere</subject><subject>Soil chemistry</subject><subject>Soil composition</subject><subject>Soil conditioners</subject><subject>Soil microorganisms</subject><subject>Soil science</subject><subject>Soil Science & Conservation</subject><subject>Soil solution</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. Amendments</subject><subject>Vermiculite</subject><subject>Water and solute dynamics</subject><subject>X-ray diffraction</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9Uctq3DAUNaWFTtN-QBcFQyl040QvS_IyhLQJBLpJIDuhka9mNMiWq2sv2q-vXIdQsigC6UrnwUGnqj5Sck4JURdIKSWiIZQ3VGrSyFfVjraKNy3h8nW1I4Szhqju8W31DvFE1juVu-pwG2OYoZ6zHdGnPNg5pLG2Y19PabaIYRnqDBEsQr1MBXJHOx4A61DGNEwJw19F8vV8hDofw-80HSFDjSnEssVlxd9Xb7yNCB-ezrPq4dv1_dVNc_fj--3V5V3jhCBz01q-l05qzto911J6xu1eAfGOgNBOAHRUSyd6z3tHBONEaGEFE7RzPXjgZ9XXzXfK6ecCOJshoIMY7QhpQUOF4FwxpmShfn5BPaUljyVdYXEpddspUljnG-tgI5gw-lS-ypXVwxBcGsGH8n7J2xKhk1oXAd0ELifEDN5MOQw2_zKUmLUrs3VlSldm7cqsUb48RbHobPSlDBfwWciUUqJt1zBs42GBSgv5n8j_Mf-0iU44p_xsKljXMkU7_gdcDK4T</recordid><startdate>20131001</startdate><enddate>20131001</enddate><creator>Vetterlein, Doris</creator><creator>Kühn, Thomas</creator><creator>Kaiser, Klaus</creator><creator>Jahn, Reinhold</creator><general>Springer</general><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>IQODW</scope><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>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></search><sort><creationdate>20131001</creationdate><title>Illite transformation and potassium release upon changes in composition of the rhizophere soil solution</title><author>Vetterlein, Doris ; Kühn, Thomas ; Kaiser, Klaus ; Jahn, Reinhold</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c440t-5a3b6c68325b3866f23ab7e0fc0e48c4ee9186c4df3dc04230484a42419cdefe3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Agricultural soils</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Animal, plant and microbial ecology</topic><topic>Biogeochemistry</topic><topic>Biological and medical sciences</topic><topic>Biomedical and Life Sciences</topic><topic>Cations</topic><topic>Chemical properties</topic><topic>Clay soils</topic><topic>Ecology</topic><topic>Environmental aspects</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>Identification and classification</topic><topic>Illite</topic><topic>Life Sciences</topic><topic>Minerals</topic><topic>Physical properties</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Plant Physiology</topic><topic>Plant roots</topic><topic>Plant Sciences</topic><topic>Plants</topic><topic>Potassium</topic><topic>Regular Article</topic><topic>Rhizosphere</topic><topic>Soil chemistry</topic><topic>Soil composition</topic><topic>Soil conditioners</topic><topic>Soil microorganisms</topic><topic>Soil science</topic><topic>Soil Science & Conservation</topic><topic>Soil solution</topic><topic>Soil-plant relationships. Soil fertility</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>Vermiculite</topic><topic>Water and solute dynamics</topic><topic>X-ray diffraction</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Vetterlein, Doris</creatorcontrib><creatorcontrib>Kühn, Thomas</creatorcontrib><creatorcontrib>Kaiser, Klaus</creatorcontrib><creatorcontrib>Jahn, Reinhold</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>Proquest Central</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vetterlein, Doris</au><au>Kühn, Thomas</au><au>Kaiser, Klaus</au><au>Jahn, Reinhold</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Illite transformation and potassium release upon changes in composition of the rhizophere soil solution</atitle><jtitle>Plant and soil</jtitle><stitle>Plant Soil</stitle><date>2013-10-01</date><risdate>2013</risdate><volume>371</volume><issue>1/2</issue><spage>267</spage><epage>279</epage><pages>267-279</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Aims and background Release of 'non-exchangeable' potassium (K) from interlayers of illite is diffusioncontrolled and has been shown to depend on the solution concentration of Ê and other cations (Ca²⁺, Mg²⁺, NH₄⁺). Methods We analysed changes in soil solution concentrations of K and competing cations in situ at different distances from the root surface over time and related them to the transformation of illite, as revealed by X-ray diffraction, and chemical measures of differently bound K. Results and Conclusions Within 49 and 98 days, respectively, 6.4 and 14.4 % of the illite's total K was released upon contact with the root system. Mixed layered minerals increased from 33 (0 d) to 35 (49 d) to 40 % (98 d). Release of K from interlayers and the transformation of illite occurred at soil solution K concentrations close to the threshold of 80 µM suggested earlier. Concentrations of Ca and Mg increased with decreasing distance from the root surface, promoting the release of K. The NaBPh₄ method supposed to determine 'non-exchangeable' K extracted only 1/3 of the total K from illite.</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1007/s11104-013-1680-6</doi><tpages>13</tpages></addata></record> |
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| subjects | Agricultural soils Agronomy. Soil science and plant productions Animal, plant and microbial ecology Biogeochemistry Biological and medical sciences Biomedical and Life Sciences Cations Chemical properties Clay soils Ecology Environmental aspects Fundamental and applied biological sciences. Psychology General agronomy. Plant production Identification and classification Illite Life Sciences Minerals Physical properties Physics, chemistry, biochemistry and biology of agricultural and forest soils Plant Physiology Plant roots Plant Sciences Plants Potassium Regular Article Rhizosphere Soil chemistry Soil composition Soil conditioners Soil microorganisms Soil science Soil Science & Conservation Soil solution Soil-plant relationships. Soil fertility Soil-plant relationships. Soil fertility. Fertilization. Amendments Vermiculite Water and solute dynamics X-ray diffraction |
| title | Illite transformation and potassium release upon changes in composition of the rhizophere soil solution |
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