DC pole | Wartość | Język |
dc.contributor.author | Pierwoła, Jolanta | - |
dc.contributor.author | Ciesielczuk, Justyna | - |
dc.contributor.author | Misz-Kennan, Magdalena | - |
dc.contributor.author | Fabiańska, Monika | - |
dc.contributor.author | Bielińska, A. | - |
dc.contributor.author | Kruszewski, Ł. | - |
dc.date.accessioned | 2020-04-07T05:43:42Z | - |
dc.date.available | 2020-04-07T05:43:42Z | - |
dc.date.issued | 2018 | - |
dc.identifier.citation | "International Journal of Coal Geology" Vol. 197 (2018), s. 1-19 | pl_PL |
dc.identifier.issn | 0166-5162 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/13463 | - |
dc.description.abstract | The Wełnowiec municipal dump, Katowice, Poland, rehabilitated with coal waste, is self-heating and igniting.
This paper presents a novel application of the use of electrical- and resistivity geophysical methods in the investigation
of burning coal waste to help explain why the heating occurred. Geoelectrical methods allowed the
internal structure of the dump to be revealed, and the municipal wastes and their rehabilitation cover containing
coal waste to be differentiated. Instead of a planned 2.2-m-thick multi-barrier system, the cover consists of
irregularly distributed material of varying thickness (< 1 to 8 m) and organic carbon content (> 5%). This
caused the fire to arise 3–4 years after the coal waste deposition. In areas where the rehabilitation layer is<3m
thick, a landslide enabled oxygen access, initiating self-heating. Changes in conductivity clearly identify sites of
active burning where measured conductivity values are more than twice those for parts of the dump with no
thermal activity. Field observations in particular, complemented to a degree by petrographic, mineralogical and
geochemical data, enabled four types of heating zones to be distinguished, namely, (1) initial zones of fire
overtaking new volumes of coal waste, (2) active zones with temperatures < 400–500 °C in exhalation vents,
(3) overburned zones characterized by long-lasting high temperatures (800-900 °C) and (4) short-lived zones,
ephemeral (< 1–2 months) with temperatures between 70 and 100 °C. The geophysical methods applied could
not distinguish between these zones. The combined results strongly suggest that the use of coal waste as a
remediation layer covering waste dumps should be prohibited. Coal waste which, by its nature, is too prone to
unpredictable self-heating and self-ignition with the potential environmental consequences that follow. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/pl/ | * |
dc.subject | Self-heating | pl_PL |
dc.subject | Thermal zones | pl_PL |
dc.subject | Coal wastes | pl_PL |
dc.subject | Electrical resistivity tomography (ERT) | pl_PL |
dc.subject | Conductivity profiling (FDEM) | pl_PL |
dc.subject | Mineralogy | pl_PL |
dc.subject | Geochemistry | pl_PL |
dc.subject | Wełnowiec | pl_PL |
dc.title | Structure and thermal history of the Wełnowiec dump, Poland : a municipal dump rehabilitated with coal waste | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.1016/j.coal.2018.08.001 | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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