Bentheimer Sandstone


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Description

The effect of pore-scale heterogeneity on non-Darcy flow behaviour is investigated by means of direct flow simulations on 3-D images of Bentheimer sandstone and Estaillades carbonate. The critical Reynolds number indicating the cessation of the creeping Darcy flow regime in Estaillades carbonate is two orders of magnitude smaller than in Bentheimer sandstone, and is three orders of magnitude smaller than in the beadpack.

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Created

Sept. 28, 2015

License

ODC-BY 1.0

Digital Object Identifier

10.17612/P77P49

Data Citation

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