Estimation of Capillary‐Associated NAPL‐Water Interfacial Areas for Unconsolidated Porous Media by Kinetic Interface Sensitive (KIS) Tracer Method

Author:

Tatomir Alexandru12,Gao Huhao1ORCID,Abdullah Hiwa1,Pötzl Christopher3,Karadimitriou Nikolaos4ORCID,Steeb Holger4ORCID,Licha Tobias5,Class Holger6,Helmig Rainer6ORCID,Sauter Martin17ORCID

Affiliation:

1. Department of Applied Geology Geoscience Centre of the University of Göttingen Göttingen Germany

2. Independent Researcher Göttingen Germany

3. Department of Structural Geology and Geodynamics Geoscience Centre of the University of Göttingen Göttingen Germany

4. Department of Structural Engineering University of Stuttgart Stuttgart Germany

5. Department of Applied Geology Institute of Geology, Mineralogy and Geophysics Ruhr University Bochum Bochum Germany

6. Department of Hydromechanics and Modelling of Hydrosystems University of Stuttgart Stuttgart Germany

7. Leibniz Institute for Applied Geophysics Hannover Germany

Abstract

AbstractBy employing kinetic interface sensitive (KIS) tracers, we investigate three different types of glass‐bead materials and three natural porous media systems to quantitatively characterize the influence of the porous‐medium grain‐, pore‐size and texture on the specific capillary‐associated interfacial area (FIFA) between an organic liquid and water. By interpreting the breakthrough curves (BTCs) of the reaction product of the KIS tracer hydrolysis, we obtain a relation for the specific IFA and wetting phase saturation. The immiscible displacement process coupled with the reactive tracer transport across the fluid–fluid interface is simulated with a Darcy‐scale numerical model. Linear relations between the specific capillary‐associated FIFA and the inverse mean grain diameter can be established for measurements with glass beads and natural soils. We find that the grain size has minimal effect on the capillary‐associated FIFA for unconsolidated porous media formed by glass beads. Conversely, for unconsolidated porous media formed by natural soils, the capillary‐associated FIFA linearly increases with the inverse mean grain diameter, and it is much larger than that from glass beads. This indicates that the surface roughness and the irregular shape of the grains can cause the capillary‐associated FIFA to increase. The results are also compared with the data collected from literature, measured with high resolution microtomography and partitioning tracer methods. Our study considerably expands the applicability range of the KIS tracers and enhances the confidence in the robustness of the method.

Funder

Deutsche Forschungsgemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

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