Mucilage secretion and its interaction with soil, and contact reduction
Contact reduction is a mechanism by which plant roots are able to mobilise Mn from insoluble oxides in the rhizosphere. Contact between the root surface is established and develops when the mucilage produced by root cells forms a gel upon its interaction with the soil. The mucigel may not only mould...
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| Veröffentlicht in: | Plant and soil 1993-10, Vol.155 (1), p.79-82 |
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| container_title | Plant and soil |
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| creator | Uren, N.C. (Trobe Univ., La Trobe, Vic. (Australia). School of Agriculture) |
| description | Contact reduction is a mechanism by which plant roots are able to mobilise Mn from insoluble oxides in the rhizosphere. Contact between the root surface is established and develops when the mucilage produced by root cells forms a gel upon its interaction with the soil. The mucigel may not only mould to the surface of soil particles, but also may diffuse into aggregates such that the soil and root surfaces overlap. In such a zone, the apparent free space and the soil solution become one and the "right set of circumstances" to facilitate reduction and subsequent uptake of Mn and perhaps Fe are established. |
| doi_str_mv | 10.1007/BF00024988 |
| format | Article |
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In such a zone, the apparent free space and the soil solution become one and the "right set of circumstances" to facilitate reduction and subsequent uptake of Mn and perhaps Fe are established.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/BF00024988</identifier><language>eng</language><publisher>Kluwer Academic Publishers</publisher><subject>Acid soils ; Agricultural soils ; Clay soils ; EXSUDATION ; EXUDACION ; EXUDATION ; FER ; Gels ; HIERRO ; IRON ; MANGANESE ; MANGANESO ; NUTRICION DE LAS PLANTAS ; NUTRITION DES PLANTES ; Oxides ; Pedogenesis ; PLANT NUTRITION ; Plant roots ; REDUCCION ; REDUCTION ; RHIZOSPHERE ; RIZOSFERA ; Soil biochemistry ; Soil plant interactions ; Soil solution</subject><ispartof>Plant and soil, 1993-10, Vol.155 (1), p.79-82</ispartof><rights>1993 Kluwer Academic Publishers</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c270t-49ec0e709ace477788602d71d0d8583d3f5deab8d77fdec803d07a5201e43ba03</citedby><cites>FETCH-LOGICAL-c270t-49ec0e709ace477788602d71d0d8583d3f5deab8d77fdec803d07a5201e43ba03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/42939266$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/42939266$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,27901,27902,57992,58225</link.rule.ids></links><search><creatorcontrib>Uren, N.C. 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In such a zone, the apparent free space and the soil solution become one and the "right set of circumstances" to facilitate reduction and subsequent uptake of Mn and perhaps Fe are established.</description><subject>Acid soils</subject><subject>Agricultural soils</subject><subject>Clay soils</subject><subject>EXSUDATION</subject><subject>EXUDACION</subject><subject>EXUDATION</subject><subject>FER</subject><subject>Gels</subject><subject>HIERRO</subject><subject>IRON</subject><subject>MANGANESE</subject><subject>MANGANESO</subject><subject>NUTRICION DE LAS PLANTAS</subject><subject>NUTRITION DES PLANTES</subject><subject>Oxides</subject><subject>Pedogenesis</subject><subject>PLANT NUTRITION</subject><subject>Plant roots</subject><subject>REDUCCION</subject><subject>REDUCTION</subject><subject>RHIZOSPHERE</subject><subject>RIZOSFERA</subject><subject>Soil biochemistry</subject><subject>Soil plant interactions</subject><subject>Soil solution</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1993</creationdate><recordtype>article</recordtype><recordid>eNpFkEFLxDAQhYMoWFcvHgWhZ7E6SdomOerirkLVi4K3kk2ma5baSpJF_Pd2W9HT8Ob7eIdHyCmFKwogrm8XAMByJeUeSWgheFYAL_dJAsBZBkK9HZKjEDawy7RMyPJxa1yr15gGNB6j67tUdzZ1MaSui-i1GX9fLr6noXft5YhN38WBpB7tdhSOyUGj24Anv3dGXhd3L_P7rHpePsxvqswwATHLFRpAAUobzIUQUpbArKAWrCwkt7wpLOqVtEI0Fo0EbkHoggHFnK808Bm5mHqN70Pw2NSf3n1o_11TqHcT1P8TDPL5JG9C7P2fmTPFFSvLgZ9NvNF9rdfehfqpUgUMPZT_ADwaX_Q</recordid><startdate>199310</startdate><enddate>199310</enddate><creator>Uren, N.C. (Trobe Univ., La Trobe, Vic. (Australia). School of Agriculture)</creator><general>Kluwer Academic Publishers</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>199310</creationdate><title>Mucilage secretion and its interaction with soil, and contact reduction</title><author>Uren, N.C. (Trobe Univ., La Trobe, Vic. (Australia). School of Agriculture)</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c270t-49ec0e709ace477788602d71d0d8583d3f5deab8d77fdec803d07a5201e43ba03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1993</creationdate><topic>Acid soils</topic><topic>Agricultural soils</topic><topic>Clay soils</topic><topic>EXSUDATION</topic><topic>EXUDACION</topic><topic>EXUDATION</topic><topic>FER</topic><topic>Gels</topic><topic>HIERRO</topic><topic>IRON</topic><topic>MANGANESE</topic><topic>MANGANESO</topic><topic>NUTRICION DE LAS PLANTAS</topic><topic>NUTRITION DES PLANTES</topic><topic>Oxides</topic><topic>Pedogenesis</topic><topic>PLANT NUTRITION</topic><topic>Plant roots</topic><topic>REDUCCION</topic><topic>REDUCTION</topic><topic>RHIZOSPHERE</topic><topic>RIZOSFERA</topic><topic>Soil biochemistry</topic><topic>Soil plant interactions</topic><topic>Soil solution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Uren, N.C. (Trobe Univ., La Trobe, Vic. (Australia). School of Agriculture)</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Uren, N.C. (Trobe Univ., La Trobe, Vic. (Australia). School of Agriculture)</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mucilage secretion and its interaction with soil, and contact reduction</atitle><jtitle>Plant and soil</jtitle><date>1993-10</date><risdate>1993</risdate><volume>155</volume><issue>1</issue><spage>79</spage><epage>82</epage><pages>79-82</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><abstract>Contact reduction is a mechanism by which plant roots are able to mobilise Mn from insoluble oxides in the rhizosphere. Contact between the root surface is established and develops when the mucilage produced by root cells forms a gel upon its interaction with the soil. The mucigel may not only mould to the surface of soil particles, but also may diffuse into aggregates such that the soil and root surfaces overlap. In such a zone, the apparent free space and the soil solution become one and the "right set of circumstances" to facilitate reduction and subsequent uptake of Mn and perhaps Fe are established.</abstract><pub>Kluwer Academic Publishers</pub><doi>10.1007/BF00024988</doi><tpages>4</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0032-079X |
| ispartof | Plant and soil, 1993-10, Vol.155 (1), p.79-82 |
| issn | 0032-079X 1573-5036 |
| language | eng |
| recordid | cdi_crossref_primary_10_1007_BF00024988 |
| source | Jstor Complete Legacy; SpringerLink Journals |
| subjects | Acid soils Agricultural soils Clay soils EXSUDATION EXUDACION EXUDATION FER Gels HIERRO IRON MANGANESE MANGANESO NUTRICION DE LAS PLANTAS NUTRITION DES PLANTES Oxides Pedogenesis PLANT NUTRITION Plant roots REDUCCION REDUCTION RHIZOSPHERE RIZOSFERA Soil biochemistry Soil plant interactions Soil solution |
| title | Mucilage secretion and its interaction with soil, and contact reduction |
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