Distribution and affinity of trace elements in Samaleswari coal, Eastern India
| Autor: | Debashis Chatterjee, Debasree Saha, D. Chatterjee, Anita Kumari, Sanchita Chakravarty, M. Raviathul Basariya, Jishnu Adhikari, Amit K. Kundu, Debasish Shome |
|---|---|
| Rok vydání: | 2016 |
| Předmět: |
020209 energy
General Chemical Engineering Energy Engineering and Power Technology chemistry.chemical_element Mineralogy 02 engineering and technology engineering.material 010502 geochemistry & geophysics 01 natural sciences Apatite Sedimentary depositional environment Siderite chemistry.chemical_compound Stratigraphic section 0202 electrical engineering electronic engineering information engineering Kaolinite Coal 0105 earth and related environmental sciences business.industry Organic Chemistry Sulfur Fuel Technology chemistry visual_art Illite visual_art.visual_art_medium engineering business |
| Zdroj: | Fuel. 181:376-388 |
| ISSN: | 0016-2361 |
| Popis: | Coal samples from a borehole in the Samaleswari open cast coal block (S-OCB) have been collected. A chemical data set ( n = 17) (proximate parameters, sulfur contents, mineral composition, trace and major element oxide concentrations) has been generated to evaluate the origin of trace elements in a vertical sequence through the stratigraphic column (∼300 m). The variations of volatile matter and fixed carbon indicate that the rank of the coal in the stratigraphic section studied increases from lignite (∼50% VM daf ) at the top to high-volatile bituminous (∼25% VM daf ) at the base, which reflects a more or less progressive increase in metamorphism from younger to older coal horizons. The major minerals present in the samples are quartz and kaolinite, followed by illite; the minor constituents are siderite, apatite and rutile. The mineralogical variations are primarily related to depth, with depositional environment having a significant role in the succession. In the studied borehole concentrations of the three major element oxides, SiO 2 , Al 2 O 3 and Fe 2 O 3 , reflect the abundance of the minerals. The study indicates a systematic increase in the concentration of some trace elements (Se, Be, Sb) with depth. These elements have no similarity in trend to ash or pyritic sulfur but have strong association with fixed carbon (dry, ash-free). Two other trace elements, Co and Mn, more or less decrease in concentration in the older coal horizons, and have a significant association with ash. Another group of trace elements (As, Pb, Cd, Cu, Ni and Zn) has a sudden increase in concentration at a particular depth. These trace elements also show a similar vertical trend to pyritic sulfur. The work is further supported by the use of statistical tools (correlation coefficient, hierarchical cluster and linear multiple regression) which suggest several possible affinities of the trace elements such as inorganic, organic and multiple. Among the analyzed trace elements Co, Mn, Cd, Pb, As, Ni, Cu, Zn display principally an inorganic affinity, whereas Be, Se and Sb show an organic affinity. The variation in concentration of some trace elements (Be, Se, Sb) appears from the study to be a consequence of rank advance. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|
Full Text from ScienceDirect