『Abstract
A strain of thermophilic fungus Aspergillus fumigatus
was cultured with K-bearing minerals to determine if microbe-mineral
interactions enhance the release of mineralic potassium. Experiments
were carried out in two settings, one with the mineral grains
and the fungal cells in direct contact, and the other employing
a membrane (pore size 0.22μm) to separate the two. Measurements
over a period of 30 days showed that, irrespective of the experimental
setup, the concentration of free K in the culture was drastically
higher than those in any of the control experiments where no living
organism was present. Moreover the occurrence of mineral-cell
physical contact enhanced potassium release by an additional factor
of 3 to 4 in comparison to the separation experiments. For contact
experiments, Electron Probe Microanalysis revealed the formation
of mycelium-mineral aggregates, and Atomic Force Microscopy imaging
further indicated the possible ingestion of mineral particles
by the fungus cells. Contrasting to what was observed and expected
in control experiments, the potassium solubilization rate showed
a positive dependence upon pH when fungi and minerals were mixed
directly, and exhibited no correlations with solution acidity
if cell-rock contact was restrained. These results appear to suggest
that A. fumigatus promoted potassium release by means of
at least three likely routes, one through the complexation of
soluble organic ligands, another appealing to the immobile biopolymers
such as the insoluble components of secretion, and the third related
to the mechanical forces in association with the direct physical
contact between cells and mineral particles.
Keywords: Microbe-mineral interaction; Mineral weathering and
dissolution; Thermophilic fungus; Aspergillus fumigatus;
K-feldspar; Illite; Potassium solubilization and release』
1. Introduction
2. Materials and methods
2.1. Isolation, selection, and identification of fungal species
2.2. Mineral phases
2.3. Experimental settings for microbe-mineral interactions
2.4. Experimental sample analysis
3. Experimental results
3.1. Release of K during fungus-rock interactions
3.2. Formation of mycelium-mineral aggregates
4. Discussion
4.1. Dependence of K solubilization kinetics upon H and time
4.2. Importance and implications of the fungus-mineral physical
interactions
5. Conclusions
Acknowledgments
References