2018
DOI: 10.1007/s12665-018-7484-5
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Visualization of gaseous and dissolved CO2 migration in porous media

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Cited by 4 publications
(1 citation statement)
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“…Meanwhile, the hydrate formation rate is limited by CO 2 diffusion through water, which is determined by gas pressure, temperature, and the pore structure in water-saturated porous media. For clayey-silt sediments with small grain sizes and pores, the CO 2 diffusion is slower than that in the sandstone and artificial samples (Kim et al., 2018).…”
Section: Resultsmentioning
confidence: 99%
“…Meanwhile, the hydrate formation rate is limited by CO 2 diffusion through water, which is determined by gas pressure, temperature, and the pore structure in water-saturated porous media. For clayey-silt sediments with small grain sizes and pores, the CO 2 diffusion is slower than that in the sandstone and artificial samples (Kim et al., 2018).…”
Section: Resultsmentioning
confidence: 99%