Effect of Bacillus subtilis on granite weathering: A laboratory experiment

Abstract We performed a comparative experiment to investigate: (1) how the ubiquitous soil bacterium Bacillus subtilis weathers granite; and (2) which granite-forming minerals weather more rapidly via biological processes. Batch system experiments (granite specimen in a 500 ml solution including NaCl, glucose, yeast extract and bacteria B. subtilis at 27 °C) were carried out for 30 days. Granite surfaces were observed by SEM before and after the experiment. B. subtilis had a strong influence on granite weathering by forming pits. There were 2.4 times as many pits and micropores were 2.3 times wider in granite exposed to B. subtilis when compared with bacteria-free samples. B. subtilis appear to preferentially select an optimum place to adhere to the mineral and dissolve essential elements from the mineral to live. Plagioclase was more vulnerable to bacterial weathering than biotite among the granite composing minerals.

[1]  J. Banfield,et al.  Characteristics of attachment and growth of Thiobacillus caldus on sulphide minerals: a chemotactic response to sulphur minerals? , 2000, Environmental microbiology.

[2]  M. Madigan,et al.  Brock Biology of Microorganisms , 1996 .

[3]  P. Bennett,et al.  Mineral stimulation of subsurface microorganisms: release of limiting nutrients from silicates , 2004 .

[4]  A. Vuorinen,et al.  Bacterial weathering of rapakivi granite , 1981 .

[5]  J. Fein,et al.  Experimental study of the effects of Bacillus subtilis on gibbsite dissolution rates under near-neutral pH and nutrient-poor conditions , 2000 .

[6]  P. Bezdička,et al.  Biodestruction and deferritization of quartz sands by Bacillus species , 2003 .

[7]  A. Rutenberg,et al.  Microbial response to surface microtopography: the role of metabolism in localized mineral dissolution , 2001 .

[8]  G. Sposito,et al.  Iron acquisition from hydrous Fe(III)-oxides by an aerobic Pseudomonas sp. , 1996 .

[9]  L. Warren Micro-organisms and earth systems – advances in geomicrobiology: Biofilms and metal geochemistry: the relevance of micro-organism-induced geochemical transformations , 2005 .

[10]  S. Brantley,et al.  Rates of bacteria-promoted solubilization of Fe from minerals: a review of problems and approaches , 2000 .

[11]  P. Holmes,et al.  On the kinetics and mechanism of the dissolution of pyrite in the presence of Thiobacillus ferrooxidans , 2001 .

[12]  J. Fulghum,et al.  Dissolution of well and poorly ordered kaolinites by an aerobic bacterium , 2001 .

[13]  Banfield,et al.  A new look at microbial leaching patterns on sulfide minerals. , 2001, FEMS microbiology ecology.

[14]  J. Ferry,et al.  Role of bacterial siderophores in dissolution of hornblende , 2000 .

[15]  Y. Bashan,et al.  Image analysis for quantification of bacterial rock weathering. , 2006, Journal of microbiological methods.

[16]  John L. Ingraham,et al.  Introduction to Microbiology , 1994 .

[17]  P. Dove,et al.  Investigation of bacterial-mineral interactions using Fluid Tapping Mode™ Atomic Force Microscopy , 1996 .

[18]  David L. Kirchman,et al.  Laboratory evidence for microbially mediated silicate mineral dissolution in nature , 1996 .