The Effect of Mechanical Shaking on the Rising Velocity of Bubbles in High‐Viscosity Shear‐Thinning Fluids

Author:

Seropian Gilles1ORCID,Higginbotham Kaylon1,Kennedy Ben M.1ORCID,Schaefer Lauren N.1ORCID,Walter Thomas R.2ORCID,Soldati Arianna34ORCID

Affiliation:

1. School of Earth and Environment University of Canterbury Christchurch New Zealand

2. GFZ German Research Center for Geosciences Potsdam Germany

3. Earth and Environmental Sciences Ludwig‐Maximilians‐Universität München Munich Germany

4. Department of Marine, Earth, and Atmospheric Sciences North Carolina State University Raleigh NC USA

Abstract

AbstractThe rising velocity of an air bubble in a non‐Newtonian shear‐thinning fluid at low Reynolds numbers is generally similar to the Newtonian case given by Stokes' law. However, when the shear‐thinning fluid is subject to mechanical oscillations, the rising velocity could significantly increase. Here, we present a series of experiments quantifying the rising velocity of single bubbles during shaking in very high‐viscosity (2,000–30,000 Pa·s) shear‐thinning silicone oils. Air bubbles (18–30 mm diameter) were injected in a tank mounted on a shaking table. The tank was horizontally oscillated, at accelerations between 0.4 and 2 g. We observed a small increase in the rising velocity of the shaking cases at our experimental conditions. The increase was larger when bubbles were large and accelerations were high. Larger accelerations experienced the largest observational errors and we emphasize the exploratory nature of our results. We also measured the change in bubble diameter during the oscillations and computed the shear rate at the bubble surface. Maximum shear rates were in the range of 0.04–0.08 s−1. At these shear rates, our analysis indicates that shear thinning behavior of our analog fluids is expected to be small and compete with elastic behavior. This transitional viscous/elastic regime helps explain the small and variable results of our experiments. Our results are relevant to the study of earthquake‐volcano interactions. Most crystal‐free silicate melts would exhibit a purely viscous, shear‐thinning behavior in a natural scenario. Seismically enhanced bubble rise could offer an explanation for the observed increased degassing and unrest following large earthquakes.

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

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