Released
Dataset

Ring-shear test data of glass beads 200-300 µm used for analogue experiments in the tectonic modelling labs at GFZ Potsdam and the Institute of Geophysics of the Czech Academy of Science, Prague

Cite as:

Rosenau, Matthias; Kemnitz, Helga; Pohlenz, Andre; Warsitzka, Michael; Zavada, Prokop (2022): Ring-shear test data of glass beads 200-300 µm used for analogue experiments in the tectonic modelling labs at GFZ Potsdam and the Institute of Geophysics of the Czech Academy of Science, Prague. GFZ Data Services. https://doi.org/10.5880/GFZ.4.1.2022.002

Status

I   N       R   E   V   I   E   W : Rosenau, Matthias; Kemnitz, Helga; Pohlenz, Andre; Warsitzka, Michael; Zavada, Prokop (2022): Ring-shear test data of glass beads 200-300 µm used for analogue experiments in the tectonic modelling labs at GFZ Potsdam and the Institute of Geophysics of the Czech Academy of Science, Prague. GFZ Data Services. https://doi.org/10.5880/GFZ.4.1.2022.002

Abstract

This dataset provides friction data from ring-shear tests on glass beads with a diameter of 200-300 µm used in analogue modelling of tectonic processes as a rock analogue for “weak” layers in the earth’s upper crust (e.g. Klinkmüller et al., 2016; Ritter et al., 2016; Lohrmann et al., 2003) or as “seismogenic” crust (Rudolf et al., 2022). The glass beads are characterized by means of internal friction coefficients µ and cohesion C.
According to our analysis the materials show a Mohr-Coulomb behaviour characterized by a linear failure envelope. Peak, dynamic and reactivation friction coefficients of the glass beads are µP = 0.51 , µD = 0.40, and µR = 0.44, respectively (Table 5). Cohesion of the material ranges between 40 Pa and 70 Pa. The material shows a minor rate-weakening of ~1% per ten-fold change in shear velocity v and a stick-slip behaviour at low shear velocities and at high loads.

Methods

The data presented here are derived by ring shear testing using a SCHULZE RST-01.pc (Schulze, 1994, 2003, 2008) at the Helmholtz Laboratory for Tectonic Modelling (HelTec) of the GFZ German Research Centre for Geosciences in Potsdam. The RST is specially designed to measure friction coefficients µ and cohesions C in loose granular material accurately at low confining pressures (<20 kPa) and shear velocities (<1 mm/sec) similar to sandbox experiments. In this tester, a granular bulk material layer is sheared internally at constant normal stress σN and shear velocity v while shear force and lid displacement (corresponding to density and volume change ΔV) are measured continuously. For more details see Klinkmüller et al. (2016) and Ritter et al. (2016).

Authors

  • Rosenau, Matthias;GFZ German Research Centre for Geosciences, Potsdam, Germany
  • Kemnitz, Helga;GFZ German Research Centre for Geosciences, Potsdam, Germany
  • Pohlenz, Andre;GFZ German Research Centre for Geosciences, Potsdam, Germany
  • Warsitzka, Michael;Institute of Geophysics, Czech Academy of Sciences, Prague, Czech Republic;Bundesgesellschaft für Endlagerung mbH (BGE), Peine, Germany
  • Zavada, Prokop;Institute of Geophysics, Czech Academy of Sciences, Prague, Czech Republic

Contact

  • Rosenau (Matthias) ; GFZ German Research Centre for Geosciences, Potsdam, Germany;

Contributors

HelTec - Helmholtz Laboratory for Tectonic Modelling (GFZ German Research Centre for Geosciences, Germany); Rosenau

Keywords

EPOS, TCS MSL, analogue models of geologic processes, multi-scale laboratories, property data of analogue modelling materials, analogue modelling results, software tools, Cohesion, Friction coefficient, deformation > shearing, fault, Microspheres > Glassy, Ring-shear tester, Cohesion, Friction coefficient, Microspheres > Glassy, Ring-shear tester, deformation > shearing, fault

Files

License: CC BY 4.0