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Experimental Investigation on the Imbibition Capacity and Its Influencing Factors in Hydrate Sediments
[Image: see text] The water generated after the dissociation of gas hydrates is spontaneously imbibed into the matrix pores. It hinders the gas–water flow and decreases the pore pressure, which is not conducive to the continuous depressurization of hydrate sediments. However, there are few research...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Chemical Society
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7315580/ https://www.ncbi.nlm.nih.gov/pubmed/32596594 http://dx.doi.org/10.1021/acsomega.0c01269 |