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- W1660746039 abstract "The chapter explains how in the past decade much progress has been made to gain a better understanding of rhizosphere processes. As used for calcium and magnesium, a similar technique can be used to measure the accumulation of ions in the rhizosphere. Marked differences in redox potential in the rhizosphere occur between plants grown in aerated soils and those grown in submerged soils. The first part of the chapter describes the sources of nitrogen supply and rhizosphere pH, the nutritional status of plants and rhizosphere pH, and the redox potential and reducing processes. The section on rhizodeposition and root exudates covers rhizodeposition and root exudates separately and elaborates the actual process taking place in each case. Mucilage may have a diversity of biological functions, including protection of root apical zones from desiccation, lubrication of the root as it moves through the soil, ion uptake (facilitation or restriction), interaction with soil particles and improving the soil–root contact, especially in dry soil, and causing aggregation of soil in the rhizosphere. The main constituents of the low-molecular-weight root exudates are sugars, organic acids, amino acids, and phenolics. Noninfecting rhizosphere microorganisms cover root colonization and phytohormone precursors. Mycorrhizas have also been explained in detail. Mycorrhizal colonization per se, and any marked change in vesicular-arbuscular mycorrhiza (VAM) root colonization of field-grown plants have implications on soil testing and on simulation models for plant-available mineral nutrients, and phosphorus in particular." @default.
- W1660746039 created "2016-06-24" @default.
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- W1660746039 date "1995-01-01" @default.
- W1660746039 modified "2023-09-26" @default.
- W1660746039 title "The Soil-Root Interface (Rhizosphere) in Relation to Mineral Nutrition" @default.
- W1660746039 doi "https://doi.org/10.1016/b978-012473542-2/50017-1" @default.
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