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Abstract

Summary

Coal wastes are produced in large amounts at various stages of coal exploitation. These rocks require special dump sites designed to store them for many years. If sufficiently large volumes of coal waste are accumulated, self-heating driven by their oxidation may occur. This process generates toxic compounds contaminating the atmosphere, water, and soil. Self-heating is a highly variable process since it depends on numerous factors. Hydropyrolysis experiments simulate well natural self-heating of coal wastes occurring in the presence of water. Pyrolysates show composition analogous to that of self-heating products what allow to predict types of contaminants formed in the process.

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/content/papers/10.3997/2214-4609.202134055
2021-09-12
2024-04-23
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References

  1. Fabiańska, M.J., Ćmiel, S.R., Misz-Kennan, M.
    2013. Biomarkers and aromatic hydrocarbons in bituminous coals of Upper Silesian Coal Basin: Example from 405 coal seam of the Zaleskie Beds (Poland). Int. J. Coal Geol.107, 96–111.
    [Google Scholar]
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