The initial fluctuations for an unstable immiscible flood are calculated using a Darcy-scale Langevin equation. The resulting amplitude is a product of a Darcy-scale dynamic term with a pore scale dispersion term. Flood velocity can minimize initial ffuctuations depending on the importance of capill
The structure and magnitude of concentration fluctuations
โ Scribed by P. C. Chatwin; Paul J. Sullivan
- Publisher
- Springer
- Year
- 1993
- Tongue
- English
- Weight
- 734 KB
- Volume
- 62
- Category
- Article
- ISSN
- 0006-8314
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