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- W129601174 abstract "During an experimental study of rhizosphere development around French Bean roots, mechanical and mineralogical modifications were recorded. The former entailed a relative decrease in material 63 — 6.3μm e.s.d. in size, probably due to disaggregation of polymineralic shale particles. The latter was most obvious in the finest (< 0.063 μm) fraction and involved a decrease in both regularly and irregularly interstratified 10/14å material: “amorphous” (extractable) A1, Fe and C accumulated in the rhizosphere, whilst Si was depleted. These effects are interpreted as being due to intensified “weathering” of soil materials in the vicinity of the plant root." @default.
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- W129601174 date "1979-01-01" @default.
- W129601174 modified "2023-09-27" @default.
- W129601174 title "MODIFICATIONS TO MECHANICAL AND MINERALOGICAL COMPOSITION OF SOIL WITHIN THE RHIZOSPHERE" @default.
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- W129601174 doi "https://doi.org/10.1016/b978-0-12-325550-1.50016-1" @default.
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