Plant-soil-microorganisms interactions driving micronutrient availability in the rhizosphere

Tanja Mimmo

Faculty of Science and Technology, Free University of Bozen-Bolzano, Italy

tanja.mimmo@unibz.it

The rhizosphere is the volume of soil where the chemical (pH, redox potential, nutrient concentration and root exudates), physical (temperature, water availability and soil structure) and biological characteristics (microbial associations) are shaped by plant-microbe-soil interactions. Communications between roots and between soil microorganisms and roots, i.e. rhizosphere processes, occur and change continuously influencing for instance the nutrients availability, their soil transport and plant uptake. The main driving force of these mechanisms seems to be related to root exudation processes. Root exudates comprise in fact a number of different organic (e.g. low molecular weight and high molecular weight organic compounds) and inorganic (e.g. protons and HCO3) chemicals and can reach concentrations up to 250 mg C /g root produced of the photosynthetically fixed carbon.

Several nutrients, in particular trace elements, are mainly either adsorbed or structural components of soil minerals, i.e. the quantitatively largest fraction in soil. Root exudates might interact with the minerals leading to mineral weathering and thus to the mobilization of trace elements with a consequent increase in their plant available fraction. However, root exudates have short half-lives because of the large microbial activity at the soil–root interface, which might limit their effects on nutrient mobility and acquisition. In addition, exudates also have a selective effect on the microbial community present in the rhizosphere. The presentation provides an overview of the rhizosphere processes involved in nutrients acquisition by soil organisms (plants and microorganisms) focusing in particular on micronutrients (iron and copper). In particular, the presentation provides information on (i) nutrients availability in soils, including mineral weathering, ligand and element competition and plant-microbe competition; (ii) microbe–plant interactions, focusing on beneficial microbial communities and their association with plants, and (iii) plant–soil interactions involving the metabolic changes triggered by nutrient deficiency and the processes involved in exudate release from roots.

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