Abundance, distribution, and modes of occurrence of uranium in Chinese coals

10Citations
Citations of this article
14Readers
Mendeley users who have this article in their library.

Abstract

Due to its environmental and resource impacts, the geochemistry of uranium in coal is of both academic and practical significance. In order to give a comprehensive summary about the geochemistry of uranium in coals, the abundance, distribution, and modes of occurrence of uranium in Chinese coals were reviewed in this paper. Although some coals from southwestern and northwestern China are significantly enriched in uranium, the common Chinese coals are of a comparable uranium concentration to the world coals. The roof and floor rocks, and parting of coalbeds, or coal benches that are close to the surrounding rock are favorable hosts for uranium in one coalbed. The uranium concentrations in coals of different ages decrease in this order, e.g., Paleogene and Neogene > Late Permian > Late Triassic > Late Carboniferous and Early Permian > Late Jurassic and Early Cretaceous > Early and Middle Jurassic. Uranium in Chinese coals is mainly associated with organic matter, and is correspondingly enriched in subbituminous coal and lignite.

Cite

CITATION STYLE

APA

Chen, J., Chen, P., Yao, D., Huang, W., Tang, S., Wang, K., … Sha, J. (2017, December 1). Abundance, distribution, and modes of occurrence of uranium in Chinese coals. Minerals. MDPI AG. https://doi.org/10.3390/min7120239

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free