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Microbial Ecology of a Natural Extreme Acidic Environment: Lessons from Río Tinto

Journal Advanced Materials Research (Volumes 71 - 73)
Volume Biohydrometallurgy 2009
Edited by Edgardo R. Donati, Marisa R. Viera, Eduardo L. Tavani, María A. Giaveno, Teresa L. Lavalle, Patricia A. Chiacchiarini
Pages 13-19
DOI 10.4028/www.scientific.net/AMR.71-73.13
Citation R. Amils et al., 2009, Advanced Materials Research, 71-73, 13
Online since May, 2009
Authors R. Amils, E. González-Toril, A. Aguilera, N. Rodriguez, D. Fernández-Remolar, E. Diaz, A. García-Moyano, Jose Luis Sanz
Keywords Acidophiles, ARD, Chemolithotrophy, Iberian Pyrite Belt, Iron Cycle, Sulfur Cycle
Abstract

Rio Tinto (Iberian Pyritic Belt, SW Spain) is a natural extreme acidic environment with a rather constant acidic pH (mean pH value 2.3) and a high concentration of heavy metals. The Tinto ecosystem is under the control of iron. The geomicrobiological characterization of Río Tinto has unravelled some basic questions of biohydrometallurgical interest. The methodologies developed for this study were applied successfully to monitor different bioleaching processes of the BioMinE project.

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