期刊
GEOMICROBIOLOGY JOURNAL
卷 37, 期 2, 页码 101-109出版社
TAYLOR & FRANCIS INC
DOI: 10.1080/01490451.2019.1666194
关键词
Aspergillus; basalt; bioweathering; glass composition; proton-promoted dissolution; ligand-promoted dissolution
资金
- National Science Foundation Project of China [40573057, 41673083]
- Open Project of the State Key Laboratory of Loess and Quaternary Geology [SKLLQG1511]
Mechanisms underlying microbe-induced dissolution of basalt and its effect on glass composition remain unclear. Two powdered basalts, with a glass composition of 27 vol% (Basalt-T) and 18 vol% (Basalt-F), respectively, were inoculated with Aspergillus sp. FS-4 in Czapek medium. Changes in pH, siderophores and main dissolved elements were examined. Basalt-F led to a greater decrease in pH and higher production of siderophores than Basalt-T mainly due to the fungi activity. Element dissolution was 2 to 3 fold higher in Basalt-T than in Basalt-F, and the dissolution was non-stoichiometric for both basalts. FS-4 appears important for basalt weathering. Composition of geologic material had a considerable impact on weathering. Materials with a higher glass percentage are prone to weathering. Further quantitative evaluation is required.
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