| 2004 Denver Annual Meeting (November 7–10, 2004) | |
| Paper No. 167-7 | |
| Presentation Time: 3:00 PM-3:15 PM | ||
FLOW REGIMES ON SMOOTH FRACTURE SURFACE REPLICA | ||
|
GHEZZEHEI, Teamrat A., Earth Science Division, Lawrence Berkeley National Lab, 1 Cyclotron Rd, MS 90R1116, Berkeley, CA 94720, TAGhezzehei@lbl.gov and SALVE, Rohit, Earth Sciences Division, Lawrence Berkeley National Lab, 1 Cyclotron Road, Berkeley, CA 94720 Recent flow visualization experiments and conceptual modeling efforts enabled identification of several distinct flow regimes in unsaturated individual fractures subjected to different initial and boundary conditions. Delineation of these dissimilar flow regimes is an essential step in the development of a self-consistent conceptual model of flow for single fractures. This study is concerned with flow on relatively smooth fracture surfaces. We present theoretical constraints for the existence of some important flow regimes in idealized smooth fracture surfaces. The flow regimes considered, in the order of increasing flow rate, are: flow of adsorbed film, sliding drops, rivulet flow, stable film flow, and wavy film flow. These theoretical analyses are corroborated with observations from flow visualization experiments. | ||
|
2004 Denver Annual Meeting (November 7–10, 2004)
General Information for this Meeting | ||
| Session No. 167 Fluid Flow and Solute Transport in Fractured Rocks Colorado Convention Center: 207 1:30 PM-5:30 PM, Tuesday, November 9, 2004 Geological Society of America Abstracts with Programs, Vol. 36, No. 5, p. 392 | ||
© Copyright 2004 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||