Hydrocarbon condensates and argillites in the Eliška Mine burnt coal waste heap of the Žacléř coal district (Czech Republic): Products of high- and lowtemperature stages of self-ignition

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F18%3A00000172" target="_blank" >RIV/00025798:_____/18:00000172 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985891:_____/18:00496810

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.coal.2017.11.003" target="_blank" >http://dx.doi.org/10.1016/j.coal.2017.11.003</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.coal.2017.11.003" target="_blank" >10.1016/j.coal.2017.11.003</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Hydrocarbon condensates and argillites in the Eliška Mine burnt coal waste heap of the Žacléř coal district (Czech Republic): Products of high- and lowtemperature stages of self-ignition

Popis výsledku v původním jazyce

The Eliška Mine waste coal heap burned intensely in the 1960s and 1980s. Now, on the surface of the heap, active vents still occur from which warm air and water vapor escape. In the neighborhood of active vents, the surficial part of the heap is enriched in hydrocarbon condensates. Based on differences in optical reflectance and fluorescence color, two types of HCC were identified. These HCC are probably formed through condensation of organic pyrolysates on the heap surface in various stages of burning, and the two types of HCC most probably reflect a gradual decrease in burning temperature and progressive cooling of the heap surface.

Název v anglickém jazyce

Hydrocarbon condensates and argillites in the Eliška Mine burnt coal waste heap of the Žacléř coal district (Czech Republic): Products of high- and lowtemperature stages of self-ignition

Popis výsledku anglicky

The Eliška Mine waste coal heap burned intensely in the 1960s and 1980s. Now, on the surface of the heap, active vents still occur from which warm air and water vapor escape. In the neighborhood of active vents, the surficial part of the heap is enriched in hydrocarbon condensates. Based on differences in optical reflectance and fluorescence color, two types of HCC were identified. These HCC are probably formed through condensation of organic pyrolysates on the heap surface in various stages of burning, and the two types of HCC most probably reflect a gradual decrease in burning temperature and progressive cooling of the heap surface.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2018

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

International Journal of Coal Geology

ISSN

0166-5162

e-ISSN

—

Svazek periodika

190

Číslo periodika v rámci svazku

April

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

20

Strana od-do

146-165

Kód UT WoS článku

000431159700010

EID výsledku v databázi Scopus

2-s2.0-85035007311