Mineral weathering and mobilization of trace metals in the rhizosphere: the role of root exudates

Autor: R. TERZANO (1), L. MEDICI (2), T. MIMMO (3), N. TOMASI (4), R. PINTON (4) AND S. CESCO (3)

Publikováno v: Goldschmidt 2011-Earth, Life and Fire, pp. 2001–2001, Praga, 14-19 agosto 2011
info:cnr-pdr/source/autori:R. TERZANO (1), L. MEDICI (2), T. MIMMO (3), N. TOMASI (4), R. PINTON (4) AND S. CESCO (3)/congresso_nome:Goldschmidt 2011-Earth, Life and Fire/congresso_luogo:Praga/congresso_data:14-19 agosto 2011/anno:2011/pagina_da:2001/pagina_a:2001/intervallo_pagine:2001–2001

The mobilization of trace elements in the soil-plant system takes place essentially in the rhizosphere, where roots are intimately in contact with soil. In the rhizosphere, conditions such as pH modification, changes in red-ox potential, high concent

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http://www.cnr.it/prodotto/i/306551