Temat: sekwestracja wegla - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Impact of the capillary pressure-saturation pore-size distribution parameter on geological carbon sequestration estimates
Autorzy:: Cheng, Ch.-L.
Perfect, E.
Yu, T. E.
Gragg, M. J.
Powiązania:: https://bibliotekanauki.pl/articles/91981.pdf
Data publikacji:: 2017
Wydawca:: Główny Instytut Górnictwa
Tematy:: geological carbon sequestration
numerical modeling
capillary pressure
saturation
cost estimate
geologiczna sekwestracja węgla
modelowanie numeryczne
ciśnienie kapilarne
nasycenie
szacowanie kosztów
Opis:: Cost estimates for geologic carbon sequestration (GCS) are vital for policy and decision makers evaluating carbon capture and storage strategies. Numerical models are often used in feasibility studies for the different stages of carbon injection and redistribution. Knowledge of the capillary pressure-saturation function for a selected storage rock unit is essential in applications used for simulating multiphase fluid flow and transport. However, the parameters describing these functions (e.g. the van Genuchten m pore size distribution parameter) are often not measured or neglected compared to other physical properties such as porosity and intrinsic permeability. In addition, the use of average instead of point estimates of m for numerical simulations of flow and transport can result in significant errors, especially in the case of coarse-grained sediments and fractured rocks. Such erroneous predictions can pose great risks and challenges to decision-making. We present a comparison of numerical simulation results based on average and point estimates of the van Genuchten m parameter for different porous media. Forward numerical simulations using the STOMP code were employed to illustrate the magnitudes of the differences in carbon sequestration predictions resulting from the use of height-averaged instead of point parameters. The model predictions were converted into cost estimates and the results indicate that varying m values in GCS modeling can cause cost differences of up to hundreds of millions dollars.
Źródło:: Journal of Sustainable Mining; 2017, 16, 3; 67-72
2300-1364
2300-3960
Pojawia się w:: Journal of Sustainable Mining
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: CO2-ECBM and CO2 sequestration in Polish coal seam – experimental study
Autorzy:: Baran, P.
Zarębska, K
Krzystolik, P
Hadro, J.
Nunn, A.
Powiązania:: https://bibliotekanauki.pl/articles/91967.pdf
Data publikacji:: 2014
Wydawca:: Główny Instytut Górnictwa
Tematy:: coal
sorption
sequestration
carbon dioxide
methane
ECBM
węgiel
sorpcja
sekwestracja
dwutlenek węgla
metan
Opis:: Purpose: Methane recovery is interesting not only because of its clean combustion; it is also beneficial for the environment because of the reduction of the amount of methane emitted into the atmosphere, which is important because of methane’s significant impact on the greenhouse effect. However, desorption of methane is a slow process, significantly dependent on the coalification of coal, its porosity and petrographic composition. Injection of carbon dioxide into the coal bed under sufficient pressure might be a factor in stimulating the efficiency of this process, as – because of preferential sorption – carbon dioxide displaces methane molecules previously absorbed in the coal matrix. Methods: The measurements were made for Polish low-rank coal used for the analysis of methane recovery from Polish coal mines. Coal samples were collected from sites used for geological, sorption and petrographic research, as well as for the assessment of the reservoir’s genetic origin CH4 content. Experimental studies of sorption were performed with the use of the volumetric method at a lower and higher gas pressure. Results: The methane isothermes show more than double the reduction of adsorption along with increasing temperature. The most sig-nificant changes of sorption capacity due to temperature variations can be seen when observing the difference in the course of the hysteresis of sorption/desorption of the gas as a function of temperature. In cases where there is a temperature of 323 K, a temperature hysteresis loop might indicate larger quantities of methane trapped in the porous structure of coal. In cases of carbon dioxide as sorbate, a similar shape of sorption isotherms occurred at both temperatures, while the temperature increase caused approximately double the reduction of sorption capacity. Also the isotherm’s shape is similar for both temperatures of measurement, indicating no effect of temperature on the amount of gas within the structure of the tested coal. High-pressure isotherms of CO2 and CH4 are confirmed in the literature, proving that carbon dioxide is the gas that allows the best penetration of the internal structure of bituminous coal. The critical temperature of CO2 (304.5 K) is so high, that sorption measurements can be performed at room temperatures (293, 298 K), where activated diffusion is relatively fast. Practical implications: Understanding the sorption of gases is the primary issue, related to the exploitation of coal seams, when explaining the mechanism of gas deposition in coal seams and its relationship with outbursts of rocks and gases in mines. Originality/ value: The results indicate successful sorption of carbon dioxide in each experiment. This provides the rationale to study the application of the coal tested to obtain methane genetic origin genetic methane with the use of the CO2 injection.
Źródło:: Journal of Sustainable Mining; 2014, 13, 2; 22-29
2300-1364
2300-3960
Pojawia się w:: Journal of Sustainable Mining
Dostawca treści:: Biblioteka Nauki

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