Rock weathering by indigenous heterotrophic bacteria of Bacillus spp. at different temperature: a laboratory experiment

TLDR: In this paper, the degradation process of silicate minerals to understand the weathering processes occurring at the change temperature in the subsurface environment with organic input was investigated with psychrotrophic heterotrophic bacteria.

Abstract: The bio-weathering of basalt, granite and gneiss was experimentally investigated in this study These rock-forming minerals weathered more rapidly via the ubiquitous psychrotrophic heterotrophic bacteria With indigenous bacteria of Bacillus spp from sediments of Lake Baikal, we traced the degradation process of silicate minerals to understand the weathering processes occurring at the change temperature in the subsurface environment with organic input The bacteria mediated dissolution of minerals was monitored with solution and solid chemistry, X-ray analyses as well as microscopic techniques We determined the impact of the bacteria on the mineral surface and leaching of K, Ca, Mg, Si, Fe, and Al from silicate minerals In the samples the release of major structural elements of silicates was used as an overall indicator of silicate mineral degradation at 4°C and 18°C from five medium exchanges over 255 days of rock bioleaching The increase of temperature importantly affected the efficiency of Fe extraction from granite and basalt as well as Si extraction from granite and gneiss In comparison with elemental extraction order at 4°C, Ca was substituted first by Fe or Si It is evident that temperature influences rock microbial weathering and results in a change of elements extraction