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Discussion papers
https://doi.org/10.5194/se-2019-20
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-2019-20
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 29 Jan 2019

Research article | 29 Jan 2019

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This discussion paper is a preprint. It is a manuscript under review for the journal Solid Earth (SE).

Distinct Element geomechanical modelling of the formation of sinkhole cluster within large-scale karstic depressions

Djamil Al-Halbouni1,2, Eoghan P. Holohan3, Abbas Taheri4, Robert A. Watson3, Ulrich Polom5, Martin P. J. Schöpfer6, Sacha Emam7, and Torsten Dahm1,2 Djamil Al-Halbouni et al.
  • 1Helmholtz Centre – German Research Centre for Geosciences (GFZ), Physics of Earthquakes and Volcanoes, Telegrafenberg, Potsdam 14473, Germany
  • 2University of Potsdam, Institute of Geosciences, P.O. Box 601553, Potsdam-Golm 14415, Germany
  • 3UCD School of Earth Sciences, University College Dublin, Belfield, Dublin 4, Ireland
  • 4School of Civil, Environmental and Mining Engineering, University of Adela ide, Adelaide, South Australia 5005, Australia
  • 5Leibnitz Institute for Applied Geophysics (LIAG), Stilleweg 2, 30655 Hannover, Germany
  • 6Department for Geodynamics and Sedimentology, University of Vienna, Athanstrasse 14, 1090, Vienna, Austria
  • 7Geomechanics and Software Engineer, Itasca Consultants S.A.S, Écully, France

Abstract. The 2D Distinct Element Method (DEM) code (PFC2D_V5) is here used to simulate the evolution of subsidence-related karst landforms, such as single and clustered sinkholes, and associated larger-scale depressions. Subsurface material in the DEM model is removed by a feedback loop to produce an array of cavities; this simulates a network of subsurface groundwater conduits growing by chemical/mechanical erosion. The growth of the cavity array is coupled mechanically to the surroundings such that cavities can grow also in part by material failure at their margins, which in the limit can produce individual collapse sinkholes. Two end-member growth scenarios of the cavity array and their impact on surface subsidence were examined in the models: (1) cavity growth at the same level and at the same individual growth rate; (2) cavity growth at progressively deepening levels with varying individual growth rates. These growth scenarios are characterised by differing stress patterns across the cavity array and its overburden, which are in turn an important factor for the formation of sinkholes and uvala-like depressions. For growth scenario (1), a stable compression arch is established around the cavity array, hindering sinkhole collapse into individual cavities and favouring block-wise subsidence across the whole cavity array. In contrast, for growth scenario (2), the stress system is more heterogeneous, such that local stress concentrations exist around individual cavities leading to stress interaction. Consequently, sinkhole collapses into individual cavities occurs by shear or tensile failure of the overburden, and these sinkholes lie within a larger scale depression linked to the cavity array as a whole. The results from models with growth scenario (2), which also account for variations in mechanical properties of the overburden, are in close agreement with surface morphological and subsurface geophysical observations from a karst area on the eastern shore of the Dead Sea.

Djamil Al-Halbouni et al.
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Short summary
A 2D numerical modelling approach to simulate the mechanical formation of sinkhole cluster inside large-scale karstic depressions is presented. Different multiple cavity growth scenarios at depth are compared regarding the mechanical process and collapse style. The outcomes of the models are compared to results from remote sensing and geophysics for an active sinkhole area at the Dead Sea region.
A 2D numerical modelling approach to simulate the mechanical formation of sinkhole cluster...
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