Sorption and Desorption of CO2 and CH4 in Vitrinite- and Inertinite-Rich Polish Low-Rank Coal
Autor: | Jakub Szczurowski, Katarzyna Czerw, Katarzyna Zarębska, Paweł Baran |
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Rok vydání: | 2020 |
Předmět: |
Bituminous coal
Langmuir Materials science business.industry 020209 energy Vitrain geology.rock_type Analytical chemistry geology Sorption 02 engineering and technology 010502 geochemistry & geophysics 01 natural sciences Inertinite Desorption 0202 electrical engineering electronic engineering information engineering Coal business Vitrinite 0105 earth and related environmental sciences General Environmental Science |
Zdroj: | Natural Resources Research. 30:543-556 |
ISSN: | 1573-8981 1520-7439 |
Popis: | Low-pressure sorption tests were carried out on samples of selected Polish bituminous coal in coal–methane and coal–carbon dioxide systems. The purpose was to determine the relationship between the petrographic composition of low-rank coal and the amount of gas stored in its porous structure and desorbed from it. The influence of the degree of coalification on the amount of sorbed gas was reduced to minimum, because isotherms of deposition and evacuation of gases were determined on the base coal samples and two concentrates of lithotypes, vitrain and durain, isolated from the original coal. It was found that the sorption capacity of carbon dioxide was related to the pertographic composition, but no such correlation was observed in regard to methane. Langmuir and Dubinin–Radushkevich sorption isotherms and the modified desorption model based on Langmuir equation were chosen. The applied equations gave a very good fit to the experimental data. Calculated parameters corresponding to free adsorption energy in the Dubinin–Radushkevich equation allow concluding on the independence of its mechanism from coal petrography and on the preference of carbon dioxide sorption. Calculated adsorption equilibrium constants in Langmuir’s equation show variability with petrographic composition of coal and have lower values for methane than for carbon dioxide. It was shown that the size of the hysteresis loop depends on the petrographic composition of coal and increases with increase in vitrinite content for both sorbates, which was confirmed by values of areal hysteresis index and hysteresis parameter. |
Databáze: | OpenAIRE |
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