1. The H2 potential of the Colombian coals in natural conditions.
- Author
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Moretti, Isabelle, Bouton, Nicolas, Ammouial, Jérémie, and Carrillo Ramirez, Alejandra
- Subjects
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COAL , *COAL gasification , *HIGH temperatures , *CENOZOIC Era , *OLIVINE - Abstract
Coal gasification to manufacture dihydrogen (H 2) has long been known as a surface process. Recent works have also highlighted the H 2 generating potential of the Organic Matter (OM). The evolution of OM generates H 2 all along the process but this gas is only expected to remain as free H 2 after the maturation and expulsion of the hydrocarbons (HC) which means at a high temperature of above 200 °C. In this paper we studied the potential of three different tertiary coals from Amaga, La Jagua de Ibirico and Barrancas, all located in Colombia. Their H 2 yields were studied using a pyrolyser and the kinetic of the H 2 generation were quantified. All the studied coals are immature to early mature as source rock (SR) with large TOC content, between 66 and 83%, and good H 2 potential. The highest values were found for the Barrancas area where the potential reached 25 mg H 2 /g TOC. The temperature corresponding to the peak of H 2 generation is between 740 and 800 °C depending of the heating rate. This corresponds to the 200–300 °C for the H 2 kitchen, even if the H 2 generation starts before as already observed for continental organic rich source rock. Comparison with the other coals shows that H 2 potential is linear with TOC. In the Colombian coals, the H 2 yield in mg H 2 /g of rock is around 1/4 of the TOC content. In average, these coals have so a H 2 yield about 10 000 mmol H 2 /kg of rock, two orders of magnitude above the "best" olivines. It should nevertheless be kept in mind that the extrapolation of these laboratory data to sedimentary basins remains unconstrained and will need to be refined when well data and modelling tools are available. • The coals have significant H 2 potential in deep sedimentary basins. • High temperature open-system pyrolizer can be used to quantify these H 2 yield. • The reaction kinetic of the H 2 generation from coal is of order 1 and H 2 window generation can extend from 200 to 400 °C. • The Cenozoic Colombian coal's yield of H 2 in mgH 2 /g rock is ca ¼ of its organic carbon content in percentage. • A 80% TOC rich coal has a H 2 yield two orders of magnitude higher than that of olivines at a similar temperature of 250 °C. [ABSTRACT FROM AUTHOR]
- Published
- 2024
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