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The Gas-absorption/Chemical-reaction Method for Measuring Air-water Interfacial Area in Natural Porous Media. | LitMetric

The Gas-absorption/Chemical-reaction Method for Measuring Air-water Interfacial Area in Natural Porous Media.

Water Resour Res

Institute of Water Resources and Environment, Jilin University, Changchun 130026, P.R. China.

Published: November 2017

AI Article Synopsis

  • The GACR method, typically used in Chemical Engineering to assess gas-liquid interfacial areas, has been successfully adapted to evaluate air-water interfacial areas in natural porous media for the first time.
  • Experimental comparisons showed that the GACR method is reliable, maintaining consistent water saturation and providing accurate interfacial area measurements, with low coefficients of variation (3.5% for glass beads, 11% for sand).
  • Results indicated that GACR-derived interfacial areas closely matched those obtained through traditional methods, demonstrating that this approach is a quick, cost-effective alternative that doesn't require specialized equipment.

Article Abstract

The gas-absorption/chemical-reaction (GACR) method used in Chemical Engineering to quantify gas-liquid interfacial area in reactor systems is adapted for the first time to measure the effective air-water interfacial area of natural porous media. Experiments were conducted with the GACR method, and two standard methods (x-ray microtomographic imaging and interfacial partitioning tracer tests) for comparison, using model glass beads and a natural sand. The results of a series of experiments conducted under identical conditions demonstrated that the GACR method exhibited excellent repeatability for maintaining constant water saturation and for measurement of interfacial area (A). Coefficients of variation for A were 3.5% for the glass beads and 11% for the sand. Estimated maximum interfacial areas (A) obtained with the GACR method were statistically identical to independent measures of the specific solid surface areas of the media. For example, the A for the glass beads is 29 (±1) cm, compared to 32 (±3), 30 (±2), and 31 (±2) cm determined from geometric calculation, N2/BET measurement, and microtomographic measurement, respectively. This indicates that the method produced accurate measures of interfacial area. Interfacial areas determined with the GACR method were similar to those obtained with the standard methods. For example, As of 47 and 44 cm were measured with the GACR and XMT methods, respectively, for the sand at a water saturation of 0.57. The results of the study indicate that the GACR method is a viable alternative for measuring air-water interfacial areas. The method is relatively quick, inexpensive, and requires no specialized instrumentation compared to the standard methods.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5898451PMC
http://dx.doi.org/10.1002/2017WR021717DOI Listing

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