Solubilization of iron-containing minerals by soil microorganisms.
Eighty-eight strains of microorganisms were isolated from soils collected in northern and southern Chile, and 10 fungi which showed the highest solubilizing action upon the iron in granodiorite were then selected. These fungi were incubated with the following iron-containing minerals: augite, hornblende, biotite, magnetite, hematite, and the igneous rock granodiorite. The solubility of iron in these minerals depended on their nature, crystalline structure, the concentration of metabolic products, or all three. Complex formation could be the mechanism involved, as a strong cation-exchange resin was not able to extract Fe from culture solutions. This conclusion is also confirmed by the R(F) values obtained by thin-layer chromatography of iron-containing culture solutions.
D000164:Acremonium / Q000378:metabolism; D001230:Aspergillus / Q000378:metabolism; D002677:Chile; D002855:Chromatography, Thin Layer; D003461:Crystallography; D003470:Culture Media; D005658:Fungi / Q000254:growth & development / Q000378:metabolism*; D005670:Fusarium / Q000378:metabolism; D006851:Hydrochloric Acid; D006863:Hydrogen-Ion Concentration; D007501:Iron / Q000378:metabolism*; D008903:Minerals / Q000378:metabolism*; D009089:Mucor / Q000378:metabolism; D010407:Penicillium / Q000378:metabolism; D012988:Soil Microbiology; D012995:Solubility
D003470:Culture Media; D008903:Minerals; D007501:Iron; D006851:Hydrochloric Acid