2008
DOI: 10.1016/j.ces.2008.03.021
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From pore scale to wellbore scale: Impact of geometry on wormhole growth in carbonate acidization

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Cited by 165 publications
(124 citation statements)
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References 38 publications
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“…Moreover, estimates in the literature show significant boundary effects on core samples smaller than 1"×6", with no dependence on domain size above this critical threshold (Cohen et al, 2008). Simulations on different sized networks of sphere packs here reveal that increasing domain size decreases number of pore volumes to breakthrough.…”
Section: Model Applications: Mortar Couplingmentioning
confidence: 77%
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“…Moreover, estimates in the literature show significant boundary effects on core samples smaller than 1"×6", with no dependence on domain size above this critical threshold (Cohen et al, 2008). Simulations on different sized networks of sphere packs here reveal that increasing domain size decreases number of pore volumes to breakthrough.…”
Section: Model Applications: Mortar Couplingmentioning
confidence: 77%
“…Cohen et al (2008) found that simulations in radial geometries showed higher optimal injection rates than in linear core flood cases, suggesting that simple linear simulations are inapplicable to field conditions. Sun et al (2012) modeled a ~1 m 2 pore-scale region around a single-phase producing well coupled to larger scale Darcy blocks using over 7500 pore scale models coupled using finite-element mortars.…”
Section: Up-scaling Techniquesmentioning
confidence: 98%
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“…In that context, it has also been studied experimentally [6,11] and numerically [12][13][14][15]. In the physics community, the interest toward these systems has been sparked by classical papers of Daccord and Lenormand, which analyzed the patterns formed in a dissolving plaster and related them to other pattern-forming systems, such as diffusion-limited aggregation [16,17].…”
Section: Introductionmentioning
confidence: 99%
“…The former is defined as [23] Pe = u 0 Ds 0 φ 0 (13) and measures the ratio of the convective fluxes to the diffusive fluxes. Here u 0 is the average Darcy flux in the initial system whereas φ 0 is an initial porosity of the system.…”
Section: Governing Equationsmentioning
confidence: 99%