Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5483706 | International Journal of Coal Geology | 2017 | 17 Pages |
Abstract
The most likely explanation for the observations made in this study is that the abnormally enriched trace elements (especially Ge) in the Wulantuga and Lincang high-Ge coals are weakly bonded to organic matter, possibly occurring in the form of chelates, thus allowing them to be removed by HCl-HF. Alternatively, these elements may be associated with fine-grained minerals (or poorly crystalline mineraloids or non-mineral inorganics) that are closely associated with organic matter but are difficult to detect.
Related Topics
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Authors
Qiang Wei, Susan M. Rimmer,