the behaviour of siderite rocks in an experimental imitation of pyrometamorphic processes in coal-waste fires: upper and lower silesian case, poland

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ID: 156486
2020
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Abstract
Little is known of the influence of fluxes on the nature and the intensity of burning in coal-waste heaps. To gain some insight, two siderite samples, one each from coal-mining waste heaps in Upper- and Lower Silesian Coal Basins (Poland), were heated under identical conditions in a thermal chamber coupled to a powder X-ray diffractometer. Differences in the behaviour of siderite phase and the products of its decomposition, mainly magnetite, wüstite, and olivine, are discussed. The waste heaps sampled underwent self-heating and self-ignition catalysed by fluxes. Though the samples are unlikely to be truly representative of the Silesian basins, the heterogeneous behaviour they displayed on heating merits description and explanation, as siderite is an important widely known flux in pyrometamorphic processes.
Reference Key
kruszewski2020mineralsthe Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Łukasz Kruszewski;Justyna Ciesielczuk
Journal ecological processes
Year 2020
DOI
10.3390/min10070586
URL
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