Biotite weathering and nutrient uptake by ectomycorrhizal fungus, Suillus tomentosus, in liquid-culture experiments
By Z. Balogh‐Brunstad, C. Keller, J. Dickinson, F. Stevens, C. Li, B. Bormann. 2008
151 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Geochemistry and Petrology, Plant Science
View Paper: https://www.semanticscholar.org/paper/5b5952e751df306b90fa45305cc584b5d63e64b4
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In Earth-Surface Processes
In Geochemistry and Petrology
In Plant Science
Citations in the corpus
- Clay minerals interaction with microorganisms: a review (2017, background): “…and EPS, that bind to metals (mainly Fe and Al) and displace the equilibrium of mineral weathering towards further dissolution (Adeyemi &Gadd, 2005; Balogh-Brunstad et al., 2008); (3) element oxidation-reduction (mainly Fe, Mn, S), which promotes mineral breakdown and dissolution (Bigham et al.,…”
- Microbial Interaction with Clay Minerals and Its Environmental and Biotechnological Implications (2020, background): “Balogh-Brunstad et al. (2008) [155] showed that fungi accelerated the biotite dissolution by 100–1000 times compared to abiotic control, with mechanisms being mainly acidification of the bulk liquid and cation complexation.”
- Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “However, several authors (Balogh-Brunstad et al., 2008; Finlay et al., 2009) have suggested that higher concentrations of organic acids may accumulate within EPS matrices that are in close proximity to mineral surfaces, so that mineral dissolution is influenced, and have called for more experiments…”