| South-Central - 38th Annual Meeting (March 15–16, 2004) | |
| Paper No. 8-5 | |
| Presentation Time: 2:40 PM-3:00 PM | ||
OIL-FIELD-BRINE-INDUCED COLLOIDAL DISPERSION: A CASE STUDY FROM SOUTHEAST TEXAS | ||
|
SASSEN, Douglas S., The Department of Geology and Geophysics, Texas A&M University, College Station, TX 77843-3115, dsassen@geo.tamu.edu. The improper disposal of oil-field brine is a wide spread problem in the Gulf Coast region of the United States. Oil-field brine contamination has scarred the landscape, damaged watersheds and compromised water supplies. An additional unrecognized threat of oil-field brine contamination is colloidal dispersion. Colloidal dispersion causes the disaggregation of colloids, such as clays, by the altering of fluid and surface chemistry to create a stable suspension. Colloidal dispersion has been shown to cause: piping erosion, slope failure, increased erosion, decreases in hydraulic conductivity, degradation of soil productivity, and increased potential for transport of adsorbed contaminants. At a site in southeast Texas piping erosion features are found in conjunction with oil-field brine contamination. Neural network analysis of data from the contaminated soil indicate that elevated sodium adsorption ratios and elevated pH levels increases colloidal dispersion when pore water electrical conductivity levels are low. These results suggest that the interaction of oil-field brines with colloid mineral surfaces causes dispersion when excessive pore fluid ions are flushed from the soil. | ||
|
South-Central - 38th Annual Meeting (March 15–16, 2004)
General Information for this Meeting | ||
| Session No. 8 Engineering Geology and Hydrogeology Texas A&M University: Geology Builiding, Room 104 1:00 PM-5:00 PM, Monday, March 15, 2004 Geological Society of America Abstracts with Programs, Vol. 36, No. 1, p. 24 | ||
© 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. | ||