The DOI matches its Crossref record.
Determination of NAPL-water interfacial areas in well-characterized porous media
Abstract
The nonaqueous-phase liquid (NAPL)-water interfacial area is an important parameter which influences the rate of NAPL dissolution in porous media. The aim of this study was to generate a set of baseline data for specific interfacial area for a two-phase-entrapped NAPL-water system in well-characterized porous media and subsequently use these data to evaluate two current theoretical models. The first model tested distributes entrapped NAPL over the pore classes based on Land's algorithm and assumes the resulting blobs to be spherical. The other model is thermodynamically based, assuming that reversible work done on the system results in an increase in interfacial area, such that the area between drainage and imbibition retention curves can be related to the interfacial area. Interfacial tracer tests (IFTT) were used to measure specific entrapped NAPL (hexadecane)-water interfacial areas in columns packed with four grades (12/20, 20/30, 30/40, 40/50) of silica sand. By use of the anionic surfactant dihexylsulfosuccinate (Aerosol MA80), IFTT gave specific interfacial areas between 58 cm(-1) for the finest sand and 16 cm(-1) for the coarsest, compared to values of between 33 and 7 cm(-1) for the first model and between 19 and 5 cm(-1) for the thermodynamic model. Results from the literature suggest that nonspherical blobs shapes occur relatively frequently; hence it is reasonable to suggest that the assumption of spherical NAPL blobs may explain the underprediction by the first m…
Overview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Fluid-fluid interfacial area is a function of soil properties such as grain size, grain-size distribution, and surface roughness.
“Research has also demonstrated that fluid-fluid interfacial area is a function of soil properties such as grain size, grain-size distribution, and surface roughness (Anwar et al., 2000; Cho and Annable, 2005; Dobson et al., 2006; Brusseau et al., 2008, 2009, 2010; Peng and Brusseau, 2005).”
From Assessing the potential contributions of additional retention processes to PFAS retardation in the subsurface (2018) · cites this paper as Dobson et al., 2006
Adsorption of surfactants to NAPL-water interfaces has been measured for a variety of porous media.
“Adsorption of surfactants to NAPL-water interfaces has been measured for a variety of porous media (Saripalli et al., 1998; Cho and Annable, 2005; Dobson et al., 2006; Brusseau et al., 2008, 2009, 2010; Narter and Brusseau, 2010; McDonald et al., 2016; Zhong et al., 2016).”
From Assessing the potential contributions of additional retention processes to PFAS retardation in the subsurface (2018) · cites this paper as Dobson et al., 2006
Data on surfactant adsorption to NAPL-water interfaces have been used to determine the impact of soil properties such as grain size on interfacial adsorption.
“These data have been used to determine the impact of soil properties such as grain size on interfacial adsorption (Cho and Annable, 2005; Dobson et al., 2006; Brusseau et al., 2009, 2010).”
From Assessing the potential contributions of additional retention processes to PFAS retardation in the subsurface (2018) · cites this paper as Dobson et al., 2006
Citations
Cites
No references could be resolved yet.
Research works printed but not linked: 30
- Mackay D. M., 1985, Environ. Sci. Technol., 19, 392, 10.1021/es00135a001 · DOI
- Zhou D., 2000, Transport. Porous Med., 39, 255, 10.1023/A:1006693126316 · DOI
- Hamed M. M., 2000, Environ. Modell. Software, 15, 450, 10.1016/S1364-8152(00)00022-0 · DOI
- Knutson C. E., 2001, Water Resour. Res., 37, 2963, 10.1029/2001WR000587 · DOI
- Powers S. E., 1994, J. Contam. Hydrol., 16, 33, 10.1016/0169-7722(94)90070-1 · DOI
- Chrysikopoulos C. V., 1998, J. Contam. Hydrol., 31, 21, 10.1016/S0169-7722(97)00053-3 · DOI
- Garg S., 1999, J. Contam. Hydrol., 36, 331, 10.1016/S0169-7722(98)00149-1 · DOI
- Miller C. T., 1990, Water Resour. Res., 26, 2796, 10.1029/WR026i011p02783 · DOI
- Bradford S. A., 1997, J. Contam. Hydrol., 27, 105, 10.1016/S0169-7722(96)00048-4 · DOI
- Skopp J, 1985, Soil Sci. Soc. Am. J., 49, 1331, 10.2136/sssaj1985.03615995004900060001x · DOI
- Reeves P. C., 1996, Water Resour. Res., 32, 2358, 10.1029/96WR01105 · DOI
- Gvirtzman H., 1991, Water Resour. Res., 27, 1176, 10.1029/91WR00303 · DOI
- Oostrom M., 2001, Adv. Water Resour., 24, 898, 10.1016/S0309-1708(01)00017-3 · DOI
- Kankare M. V., 1996, Langmuir, 7, 14
- Anwar F. A. H. M., 2000, J. Contam. Hydrol., 43, 146
- Montemagno C. D., 1995, Geophys. Res. Lett., 22, 428
- Al-Raoush R. I., 2005, J. Contam. Hydrol., 77, 89
- Kim H., 1997, Water Resour. Res., 33, 2711
- Jain V., 2003, Environ. Sci. Technol., 37, 591, 10.1021/es020550s · DOI
- Saripalli P. K., 1998, J. Contam. Hydrol., 30, 391, 10.1016/S0169-7722(97)00052-1 · DOI · Paper page
- Kim H., 1999, J. Contam. Hydrol., 40, 94
- Schroth M. H., 1996, Soil Sci. Soc. Am. J., 60, 1339, 10.2136/sssaj1996.03615995006000050007x · DOI
- J. W. Gibbs collected works; Yale University Press: New Haven, 1948; Vol. 1.
- Ogata A., 1961, A solution of the differential equation of longditudinal dispersion in porous media. U. S. Geological Survey Professional Paper
- Leverett M. C, 1940, Trans. Inst. Min. Metall., 142, 169
- Lenhard R. J, 1992, J. Contam. Hydrol., 9, 269, 10.1016/0169-7722(92)90007-2 · DOI
- Van Genuchten M. T, 1980, Soil Sci. Soc. Am. J., 44, 898, 10.2136/sssaj1980.03615995004400050002x · DOI · Paper page
- Schroth M. H., 1995, J. Contam. Hydrol., 19, 287, 10.1016/0169-7722(95)00023-O · DOI
- Schaeffer C. E., 2000, Water Resour. Res., 36, 890
- Li Y., 1985, J. Colloid Interface Sci., 109, 472
Cited by
Sorted by citations
Brusseau, M. L. (2018) · Science of The Total Environment · doi:10.1016/j.scitotenv.2017.09.065 · Cited by 306
Adsorption of PFOA at the air-water interface during transport in unsaturated porous media
Lyu, Y., Brusseau, M. L., Chen, W., Yan, N., Fu, X., & Lin, X. (2018) · Environmental Science & Technology · doi:10.1021/acs.est.8b02348 · Cited by 259
Brusseau, M. L. (2019) · Water Research · doi:10.1016/j.watres.2018.12.057 · Cited by 157
Brusseau, M. L. (2019) · Environmental Pollution · doi:10.1016/j.envpol.2019.113102 · Cited by 93
Metadata
- Authors
- Dobson, R., Schroth, M. H., Oostrom, M., & Zeyer, J.
- Affiliations
- Institute of Terrestrial Ecology, ETH Zurich, 8092 Zurich, Switzerland, and Pacific Northwest National Laboratory, P. O. Box 999, MS K9-33, Richland, Washington 99352
- Venue
- Environmental Science & Technology
- Publisher
- American Chemical Society (ACS)
- Published
- 2005-12-24
- Volume
- 40
- Issue
- 3
- Pages
- 815-822
- ISSN
- 0013-936X
- 1520-5851
- Cited by
- 46
- References
- 0
- Language
- en
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review