Simulation of Geophysical Fluid Flow Under Microgravity - 2 (Geoflow-2) - 09.17.14

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Simulation of Geophysical Fluid Flow under Microgravity - 2 (Geoflow-2) studies heat and fluid flow currents within the Earth's mantle. Geoflow-2 aims to improve computational methods that scientists and engineers use to understand and predict the processes in the Earth's mantle that lead to volcanic eruptions, plate tectonics and earthquakes.

Science Results for Everyone

Following on Geoflow-1, this experiment investigated temperature-dependent fluid viscosity properties using numerical simulations in three-dimensions. The flow patterns differed between Geoflow-1 and Geoflow-2. In Geoflow-1, researchers observed a sheet-like thermal flow and successfully reproduced simulated convection patterns. In Geoflow-2, plume-like structures were observed. Numerical simulations do not yield this type of solution for the low viscosity contrast realized in the experiment, but using a viscosity contrast of two orders of magnitude or higher, scientists could reproduce the Geoflow-2 patterns. They concluded that nonlinear effects shift the effective viscosity ratio.

The following content was provided by Christoph Egbers, Ph.D., and is maintained in a database by the ISS Program Science Office.
Information provided courtesy of the Erasmus Experiment Archive.

Experiment Details


Principal Investigator(s)

  • Christoph Egbers, Ph.D., Brandenburg University of Technology, Cottbus, Germany

  • Co-Investigator(s)/Collaborator(s)
  • J. Srulijes, France
  • Birgit Futterer, Brandenburg University of Technology, Cottbus, Germany
  • Philippe Beltrame, Ph.D., Max-Planck-Institut fur Physik Komplexer Systeme, Dresden, Germany
  • Pascal Chossat, Centre International Rencontres Mathematiques, Marseille, France
  • Frederik Feudel, University of Potsdam, Potsdam, Germany
  • Rainer Hollerbach, Ph.D., Institute of Geophysics, Zurich, Switzerland
  • Innocent Mutabazi, University of Le Havre, Le Havre, France
  • Laurette S. Tuckerman, Ph.D., Ecole Superieure de Physique et de Chimie Industrielles, Paris, France
  • D Breuer, Institute of Planetary Research, Berlin, Germany

  • Developer(s)
    Information Pending
    Sponsoring Space Agency
    European Space Agency (ESA)

    Sponsoring Organization
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    Research Benefits
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    ISS Expedition Duration
    September 2010 - September 2012

    Expeditions Assigned

    Previous ISS Missions
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    Experiment Description

    Research Overview

    • Simulation of Geophysical Fluid Flow Under Microgravity - 2 (Geoflow-2) investigates the flow of a fluid between two rotating spheres, where the smaller sphere sits inside of the larger sphere. The spheres rotate about a common axis under the influence of a simulated gravitational force field (the gravity field simulated with an applied electric field).

    • Geoflow-2 differs from Geoflow-1 in that the fluid in Geoflow-2 is designed to change its inherent resistance to flow (viscosity) when the temperature of the fluid changes.

    • This experimental design will help to show how fluids flow in a configuration similar to the one found in the liquid nuclei of planets.

    • Understanding the fluid flow in this experiment will not only enhance computer models in predicting earthquakes and volcanic eruptions, but also could be useful in a variety of engineering applications, such as improving spherical gyroscopes and bearings, and centrifugal pumps.

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    Space Applications
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    Earth Applications
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    Operational Requirements
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    Operational Protocols
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    Results/More Information
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    Results Publications

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    Ground Based Results Publications

      Futterer B, Dahley N, Koch S, Scurtu N, Egbers C.  From isoviscous convective experiment ‘GeoFlow I’ to temperature-dependent viscosity in ‘GeoFlow II’—Fluid physics experiments on-board ISS for the capture of convection phenomena in Earth's outer core and mantle. Acta Astronautica. 2012; 71: 11-19. DOI: 10.1016/j.actaastro.2011.08.005.

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    ISS Patents

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    Related Publications

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    image Geoflow-2 models convection in the Earth's mantle (Image courtesy of Brandenburgische Technische Universit├Ąt).
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    image Geoflow-2 fluid cell assembly: core unit of the experiment. The inner sphere is just visible inside outer glass. Image courtesy of Brandenburgische Technische Universit├Ąt.
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    image NASA Image: ISS029E006885 - View of printed sign saying "DO NOT TOUCH. EXPERIMENT RUNNING" in front of the FSL (Fluid Science Laboratory) rack taken by the Expedition 29 crew.
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