Analysis on Acidity and Alkalinity of Metallogenetic Environment in Penecontemporaneous Period on the Bauxite in WZD Area, Northern Guizhou, China

Tao Cui

doi:10.4028/www.scientific.net/AMR.989-994.1428

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Analysis on Acidity and Alkalinity of Metallogenetic Environment in Penecontemporaneous Period on the Bauxite in WZD Area, Northern Guizhou, China
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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 989-994Analysis on Acidity and Alkalinity of...

Analysis on Acidity and Alkalinity of Metallogenetic Environment in Penecontemporaneous Period on the Bauxite in WZD Area, Northern Guizhou, China

Abstract:

Acidity and alkalinity of metallogenetic environment in penecontemporaneous period is very important for the informing of high grade bauxite. Through the research on migration regular of elements, the position of rare earth mineral and the qualitative alternation of bauxite we found that metallogenetic environment is acidic in penecontemporaneous period, from top to bottom of the profile acidity is decreased gradually. In the acidic condition, Si and Fe moved downward but Al is relative enrichment in the middle-upper part of profile.

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Periodical:

Advanced Materials Research (Volumes 989-994)

Pages:

1428-1431

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.989-994.1428

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Online since:

July 2014

Authors:

Tao Cui*

Keywords:

Acidity, Alkalinity, Bauxite, WZD Area

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* - Corresponding Author

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