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- W2481165696 abstract "This chapter focuses on the role played by the plant roots in various physicochemical processes that determine the rhizosphere chemistry. Plant roots can modify the rhizosphere chemistry in various ways, such as by releasing and uptaking organic compounds, by gas exchange related with respiration of roots and rhizosphere microorganisms, and by root uptake as well as release of water and nutrients. Roots also modify the physical properties of the rhizosphere soil, such as aggregate stability, hydrophobicity, and numbers and size of micropores by their growth through the soil as well as presence of polymeric substances. Although the total soil content of nutrients frequently exceeds the plant requirements by several orders of magnitude, plant availability is often limited by low solubility of nutrients such as P, K, ammonium, Fe, Zn, Mn, Cu, and Mo. Nitrate is the major form of inorganic N available for plant growth in many well-aerated agricultural soils, and its uptake results in excess uptake of anions over cations, net uptake of protons, and thus an increase in rhizosphere pH. In neutral or alkaline soils, rhizosphere acidification with ammonium supply can enhance the mobilization of sparingly soluble Ca phosphates and thereby increase P uptake." @default.
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- W2481165696 date "2012-01-01" @default.
- W2481165696 modified "2023-10-12" @default.
- W2481165696 title "Rhizosphere Chemistry in Relation to Plant Nutrition" @default.
- W2481165696 doi "https://doi.org/10.1016/b978-0-12-384905-2.00014-5" @default.
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