Temat: uwęglenie - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Transient one-dimensional model of coal carbonization in a stagnant packed bed
Autorzy:: Polesek-Karczewska, S.
Kardaś, D.
Grucelski, A.
Stelmach, S.
Wardach-Święcicka, I.
Powiązania:: https://bibliotekanauki.pl/articles/240628.pdf
Data publikacji:: 2013
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: carbonization
coking process
coal charge evaporation
mass source
pyrolytic gases
uwęglenie
proces koksowania
odparowanie
źródło masy
gaz pirolityczny
Opis:: In the present paper, the one-dimensional model for heat and mass transfer in fixed coal bed was proposed to describe the thermal and flow characteristics in a coke oven chamber. For the purpose of the studied problem, the analysis was limited to the calculations of temperature field and pyrolytic gas yield. In order to verify the model, its theoretical predictions for temperature distribution during wet coal charge carbonization were compared with the measurement results found in the literature. In general, the investigation shows good qualitative agreement between numerical and experimental data. However, some discrepancy regarding the temperature characteristics at the stage of evaporation was observed.
Źródło:: Archives of Thermodynamics; 2013, 34, 2; 39-51
1231-0956
2083-6023
Pojawia się w:: Archives of Thermodynamics
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Thermal history of the Carboniferous strata in the northern part of the Intra-Sudetic Basin (SW Poland): A combined Raman spectroscopy and organic petrography study
Autorzy:: Botor, Dariusz
Toboła, Tomasz
Waliczek, Marta
Powiązania:: https://bibliotekanauki.pl/articles/1835585.pdf
Data publikacji:: 2020
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: Raman spectroscopy
vitrinite reflectance
dispersed organic matter
coalification
Lower Silesia Coal District
Bohemian Massif
spektroskopia Ramana
refleksyjność witrynitu
rozproszona materia organiczna
uwęglenie
Dolnośląskie Zagłębie Węglowe
Masyw Czeski
Opis:: Raman spectroscopy and vitrinite reflectance measurements of dispersed organic matter from Carboniferous shales in boreholes in the northern part of the Intra-Sudetic Basin were used for thermal history reconstruction. Microscopic investigations have shown that the organic matter is dominated by the vitrinite maceral group. In analysed samples, organic matter shows a varied degree of thermal alteration determined by the mean random vitrinite reflectance (VRo) ranging from 0.72% to 3.80%. Mean apparent maximum vitrinite reflectance (R’max) values reached 4.98%. The full width at half maximum of D1 and G bands in Raman spectra are well-correlated with mean VRo and R’max. Thermal maturity in the boreholes shows a regular increase with depth. Geological data combined with Raman spectroscopy and mean vitrinite reflectance results indicate that the analysed Carboniferous strata reached maximum paleotemperatures from c. 110 to c. 265°C. The regional paleogeothermal gradient in the late Paleozoic was c. 80°C/km. The Variscan heating event presumably caused a major coalification process of organic matter. The Carboniferous–Permian magmatic activity must have contributed to high heat flow, adding to the effect of sedimentary burial on the thermal maturity.
Źródło:: Acta Geologica Polonica; 2020, 70, 3; 363--396
0001-5709
Pojawia się w:: Acta Geologica Polonica
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Thermal history of the Carboniferous strata in the northern part of the Intra-Sudetic Basin (SW Poland): A combined Raman spectroscopy and organic petrography study
Autorzy:: Botor, Dariusz
Toboła, Tomasz
Waliczek, Marta
Powiązania:: https://bibliotekanauki.pl/articles/139342.pdf
Data publikacji:: 2020
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: Raman spectroscopy
vitrinite reflectance
dispersed organic matter
coalification
Lower Silesia Coal District
Bohemian Massif
spektroskopia Ramana
refleksyjność witrynitu
rozproszona materia organiczna
uwęglenie
Dolnośląskie Zagłębie Węglowe
Masyw Czeski
Opis:: Raman spectroscopy and vitrinite reflectance measurements of dispersed organic matter from Carboniferous shales in boreholes in the northern part of the Intra-Sudetic Basin were used for thermal history reconstruction. Microscopic investigations have shown that the organic matter is dominated by the vitrinite maceral group. In analysed samples, organic matter shows a varied degree of thermal alteration determined by the mean random vitrinite reflectance (VRo) ranging from 0.72% to 3.80%. Mean apparent maximum vitrinite reflectance (R’max) values reached 4.98%. The full width at half maximum of D1 and G bands in Raman spectra are well-correlated with mean VRo and R’max. Thermal maturity in the boreholes shows a regular increase with depth. Geological data combined with Raman spectroscopy and mean vitrinite reflectance results indicate that the analysed Carboniferous strata reached maximum paleotemperatures from c. 110 to c. 265°C. The regional paleogeothermal gradient in the late Paleozoic was c. 80°C/km. The Variscan heating event presumably caused a major coalification process of organic matter. The Carboniferous–Permian magmatic activity must have contributed to high heat flow, adding to the effect of sedimentary burial on the thermal maturity.
Źródło:: Acta Geologica Polonica; 2020, 70, 3; 363-396
0001-5709
Pojawia się w:: Acta Geologica Polonica
Dostawca treści:: Biblioteka Nauki

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