Characterizing pore-scale configuration of organic immiscible liquid in multiphase systems with synchrotron X-ray microtomography
Characterizing pore-scale configuration of organic immiscible liquid in multiphase systems with synchrotron X-ray microtomography
Vadose Zone Journal (May 2006) 5 (2): 641-648
- air
- Arizona
- Basin and Range Province
- chlorinated hydrocarbons
- clastic sediments
- Entisols
- fluid phase
- halogenated hydrocarbons
- high-resolution methods
- image analysis
- immiscibility
- multiphase flow
- North America
- organic compounds
- Pima County Arizona
- porosity
- porous materials
- quantitative analysis
- reactivity
- sand
- sediments
- soils
- spatial distribution
- synchrotron radiation
- techniques
- tetrachloroethylene
- three-dimensional models
- tomography
- tracers
- Tucson Arizona
- United States
- unsaturated zone
- visualization
- water
- X-ray data
- blob distribution
The objective of this study was to examine the pore-scale distribution and morphology of organic immiscible liquid in natural porous media containing three immiscible fluids. High-resolution, three-dimensional images of an organic liquid (tetrachloroethene) in both three-phase (water-air-organic liquid) and two-phase (water-organic liquid) systems were obtained using synchrotron X-ray microtomography. These data were used to quantitatively characterize the morphology of the organic liquid residing within columns packed with one of three natural, sandy porous media. Organic-liquid blobs varied greatly in both size and shape, ranging from small, single spheres (> or =0.03 mm in diameter) to large, amorphous ganglia with mean lengths of 4 to 5 mm. Singlets comprised the greatest number of blobs, whereas the large ganglia, while much fewer in number, comprised the majority of the organic-liquid surface area and volume. A significant portion of the organic liquid in the three-phase systems was observed to exist as lenses and films in contact with air. These features were not observed in the two-phase water-organic liquid systems. The median of the blob-frequency distributions was smaller and the variance larger for the three-phase systems. In addition, the global specific surface areas of the organic liquid were greater for the three-phase systems. These differences are attributed to the presence of the organic-liquid lenses and films for the three-phase systems.