AN INVESTIGATION OF SATURATION-CAPILLARY PRESSURE RELATIONS IN 2-FLUID AND 3-FLUID SYSTEMS FOR SEVERAL NAPLS IN DIFFERENT POROUS-MEDIA

Citation
Rd. Busby et al., AN INVESTIGATION OF SATURATION-CAPILLARY PRESSURE RELATIONS IN 2-FLUID AND 3-FLUID SYSTEMS FOR SEVERAL NAPLS IN DIFFERENT POROUS-MEDIA, Ground water, 33(4), 1995, pp. 570-578
Citations number
13
Categorie Soggetti
Geosciences, Interdisciplinary","Water Resources
Journal title
ISSN journal
0017467X
Volume
33
Issue
4
Year of publication
1995
Pages
570 - 578
Database
ISI
SICI code
0017-467X(1995)33:4<570:AIOSPR>2.0.ZU;2-6
Abstract
Lack of constitutive data has impeded efforts to model the subsurface transport of organic-liquid contaminants. To help fill this need, func tional relationships between fluid saturations and capillary pressures were obtained using a unique fluid-retention cell. The functional rel ationships between water saturations and NAPL-water capillary pressure s, and between total-liquid saturations and air-NAPL capillary presure s in two- and three-fluid phase systems were measured directly during monotonic drainage of a fine quartz sand and a nonswelling loam soil. Additionally, measurements were made between water saturations and air -water capillary pressures for an air-water fluid system in both porou s media. The NAPLs investigated were Soltrol 170(R), toluene, and tric hloroethylene (TCE). Following the:measurements, the two- and three-fl uid retention relations were compared to test the validity of extendin g two-phase saturation-pressure (S-P) relations to three-fluid systems . Good agreement was observed between the two- and three-fluid data fo r Soltrol 170(R), toluene, and TCE in both porous media. An S-P scalin g format for two- and three-phase systems was also evaluated. Results indicate that a single multiphase retention function is suitable for d escribing two- and three-phase S-P relations in similar porous media; however, it is unclear whether the scaling factors can be predicted a priori from ratios of interfacial tensions.