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The interaction of fungus with calcite and the effects on aqueous Geochemistry in karst systems
Weiguo Hou;  Chuanwei Dou;  Bin Lian;  Hailiang Dong
2013
Source PublicationCarbonates and Evaporites
Volume28Issue:4Pages:413-418
Abstract

Geochemical variations induced by the interaction of fungus and calcite were studied. The results showed that the fungal metabolic activities could accelerate the calcite dissolution rate, and dissolution continued even when the solution was supersaturated with respect to calcite. The calcite dissolution rate was also influenced by solution chemistry, such as pH and the concentration of HCO−3HCO3−. Based on these results, the importance of fungal activity in the formation of karst geomorphology was discussed.

KeywordFungus Calcite Dissolution Geochemical Variations Sic
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/11032
Collection环境地球化学国家重点实验室
Affiliation1.State Key Laboratory of Biogeology and Evironmental Geology, School of Earth Sciences and Resources, China University of Geosciences, Beijing, China
2.State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China
3.Department of Geology, Miami University, Oxford, OH, USA
Recommended Citation
GB/T 7714
Weiguo Hou;Chuanwei Dou;Bin Lian;Hailiang Dong. The interaction of fungus with calcite and the effects on aqueous Geochemistry in karst systems[J]. Carbonates and Evaporites,2013,28(4):413-418.
APA Weiguo Hou;Chuanwei Dou;Bin Lian;Hailiang Dong.(2013).The interaction of fungus with calcite and the effects on aqueous Geochemistry in karst systems.Carbonates and Evaporites,28(4),413-418.
MLA Weiguo Hou;Chuanwei Dou;Bin Lian;Hailiang Dong."The interaction of fungus with calcite and the effects on aqueous Geochemistry in karst systems".Carbonates and Evaporites 28.4(2013):413-418.
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