2021
DOI: 10.1016/j.enggeo.2021.106059
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Porosity and permeability variability across a chalk reservoir in the Danish North Sea: Quantitative impacts of depositional and diagenetic processes

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Cited by 22 publications
(5 citation statements)
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“…For each of these sets, four permeability fields are generated with different correlation lengths in the x-direction equal to 1, 5, 50 and 200 m. In total, 3 × 4 = 12 permeability fields are made. The porosity is calculated using eq Due to the presence of heterogeneity, the local fluctuation of the velocity occurs in the reservoir.…”
Section: Methodsmentioning
confidence: 99%
“…For each of these sets, four permeability fields are generated with different correlation lengths in the x-direction equal to 1, 5, 50 and 200 m. In total, 3 × 4 = 12 permeability fields are made. The porosity is calculated using eq Due to the presence of heterogeneity, the local fluctuation of the velocity occurs in the reservoir.…”
Section: Methodsmentioning
confidence: 99%
“…The computational domain is extracted from an SEM image of chalk (Figure 4a) 43 to resemble the size and shape distributions of natural chalk grains. The resulting geometry contains a heterogeneous network of pore size and shape, including dead-end pores, narrow pore throats, and large pores with high connectivity.…”
Section: Wettability Alterationmentioning
confidence: 99%
“…Chalk is a microporous rock built of very small particles (µm radius) from phytoplankton microorganisms. The rock has low permeability (below 10 mD) [32]. In [33], it was found that "newly deposited chalk has interparticle porosity between the sediment grains, and intraparticle porosity within shells of microfossils", but the final value depends on depth, continuous burial, load of the increasing overburden, type of pore water and sediment relationships, presence of stylolites, and pressure dissolution.…”
Section: Porositymentioning
confidence: 99%