FLUID FLOW AND MIXING IN ROUGH-WALLED FRACTURE INTERSECTIONS

dc.contributor.authorJohnson J.
dc.contributor.authorBrown S.
dc.contributor.authorStockman H.
dc.date.accessioned2025-02-22T06:18:01Z
dc.date.available2025-02-22T06:18:01Z
dc.date.issued2006
dc.description.abstractFracture intersections play a basic role in contaminant transport through fracture networks because they allow different fluids to mix and disperse along the flow paths. We use experimental and numerical methods to understand and improve predictions of these phenomena. Laboratory experiments of mixing between two miscible fluids were performed within an artificial, rough-walled fracture intersection made of textured glass. We also develop a numerical model of mixing based on local application of streamline routing within the irregular aperture distribution of the intersection. This model shows good agreement with the laboratory experiments, both in the amount of average mixing and in the spatial distribution of dye streamlines. The numerical model is used to generalize our results based on aperture statistics, and shows that mixing is significantly affected by how well apertures correlate across the intersection, especially as fractures are closed. We conclude that flow channelization through rough-walled intersecting fractures significantly enhances physical mixing compared to intersecting parallel plates. Relative to transport through parallel plate aperture networks, surface roughness may reduce solute dilution and increase solute dispersion. Copyright 2006 by the American Geophysical Union.
dc.identifierhttps://www.elibrary.ru/item.asp?id=29644571
dc.identifier.citationJournal of Geophysical Research: Solid Earth, 2006, 111, 12, B12206
dc.identifier.doi10.1029/2005JB004087
dc.identifier.issn2169-9313
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/48089
dc.titleFLUID FLOW AND MIXING IN ROUGH-WALLED FRACTURE INTERSECTIONS
dc.typeСтатья

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