H<sub>2</sub> Transport in Sedimentary Basin
Natural hydrogen is generated by fairly deep processes and/or in low-permeability rocks. In such contexts, fluids circulate mainly through the network of faults and fractures. However, hydrogen flows from these hydrogen-generating layers can reach sedimentary rocks with more typical permeability and...
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| Päätekijät: | , , , |
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| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
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MDPI AG
2025-08-01
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| Sarja: | Geosciences |
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| Linkit: | https://www.mdpi.com/2076-3263/15/8/298 |
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