X-ray photoelectron evidence for bacteria-enhanced dissolution of hornblende
By B. Kalinowski, L. Liermann, Susan L. Brantley, A. Barnes, Carlos Pantano. 2000
151 citations recorded by the source corpus.
Subfields: Biomedical Engineering, Environmental Chemistry, Geochemistry and Petrology
View Paper: https://www.semanticscholar.org/paper/b3d748e4aefd0ddaabb07c67da552cfd356df1fe
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Citations in the corpus
- Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “…substantial amounts of Fe, such as hornblende and biotite, show enhanced dissolution rates in the presence of bacterial or fungal siderophores (Kalinowski et al., 2000; Sokolova et al., 2010), and attachment of microorganisms to the mineral surfaces appears to lead to greater dissolution of…”
- Siderophores in environmental research: roles and applications (2014, background): “The general mechanism is that the Fe(III)– siderophore complex is formed at the mineral surface and is then transferred into the surrounding soil solution and becomes available for uptake by microorganisms or plants (Kalinowski et al., 2000; Kraemer, 2004).”