Articles | Volume 10, issue 4
https://doi.org/10.5194/se-10-1219-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-10-1219-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Distinct element geomechanical modelling of the formation of sinkhole clusters within large-scale karstic depressions
Djamil Al-Halbouni
CORRESPONDING AUTHOR
Helmholtz Centre – German Research Centre for Geosciences (GFZ),
Physics of Earthquakes and Volcanoes, Telegrafenberg, Potsdam,
Germany
University of Potsdam, Institute of Geosciences, P.O. Box 601553,
Potsdam–Golm, Germany
Eoghan P. Holohan
UCD School of Earth Sciences, University College Dublin, Belfield,
Dublin, Ireland
Abbas Taheri
School of Civil, Environmental and Mining Engineering, University of
Adelaide, Adelaide, South Australia, Australia
Robert A. Watson
UCD School of Earth Sciences, University College Dublin, Belfield,
Dublin, Ireland
Ulrich Polom
Department S1 – Seismics, Gravimetry, and Magnetics, Leibnitz Institute for Applied Geophysics (LIAG), Stilleweg 2,
Hanover, Germany
Martin P. J. Schöpfer
Department for Geodynamics and Sedimentology, University of Vienna,
Athanstrasse 14, Vienna, Austria
Sacha Emam
Geomechanics and Software Engineer, Itasca Consultants S.A.S,
Écully, France
Torsten Dahm
Helmholtz Centre – German Research Centre for Geosciences (GFZ),
Physics of Earthquakes and Volcanoes, Telegrafenberg, Potsdam,
Germany
University of Potsdam, Institute of Geosciences, P.O. Box 601553,
Potsdam–Golm, Germany
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Sinkholes are round depression features in the ground that can cause high economic and life loss. On the Dead Sea shoreline, hundreds of sinkholes form each year driven by the fall of the water level and subsequent out-washing and dissolution of loose sediments. This study investigates the mechanical formation of sinkholes by numerical modelling. It highlights the role of material strength in the formation of dangerous collapse sinkholes and compares it to findings from a field site in Jordan.
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The alluvial fan of Ghor Al-Haditha (Dead Sea) is affected by subsidence and sinkholes. Different models and hypothetical processes have been suggested in the past; high-resolution shear wave reflection surveys carried out in 2013 and 2014 showed the absence of evidence for a massive shallow salt layer as formerly suggested. Thus, a new process interpretation is proposed based on both the dissolution and physical erosion of Dead Sea mud layers.
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Djamil Al-Halbouni, Eoghan P. Holohan, Abbas Taheri, Martin P. J. Schöpfer, Sacha Emam, and Torsten Dahm
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Ulrich Polom, Hussam Alrshdan, Djamil Al-Halbouni, Eoghan P. Holohan, Torsten Dahm, Ali Sawarieh, Mohamad Y. Atallah, and Charlotte M. Krawczyk
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Short summary
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The alluvial fan of Ghor Al-Haditha (Dead Sea) is affected by subsidence and sinkholes. Different models and hypothetical processes have been suggested in the past; high-resolution shear wave reflection surveys carried out in 2013 and 2014 showed the absence of evidence for a massive shallow salt layer as formerly suggested. Thus, a new process interpretation is proposed based on both the dissolution and physical erosion of Dead Sea mud layers.
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Subrosion is the subsurface leaching of soluble rocks. It is a global phenomenon and a geohazard in urban areas because it causes depressions and sinkholes. This is the case in the study area, the town of Bad Frankenhausen, in northern Thuringia, Germany. Using shear-wave seismic reflection we are able to image these structures at high resolution to a depth of ca. 100 m. We observe that the underground is strongly fractured and there are indications of cavities.
T. Dahm, P. Hrubcová, T. Fischer, J. Horálek, M. Korn, S. Buske, and D. Wagner
Sci. Dril., 16, 93–99, https://doi.org/10.5194/sd-16-93-2013, https://doi.org/10.5194/sd-16-93-2013, 2013
D. Al-Halbouni
Solid Earth Discuss., https://doi.org/10.5194/sed-5-1031-2013, https://doi.org/10.5194/sed-5-1031-2013, 2013
Preprint withdrawn
Related subject area
Subject area: The evolving Earth surface | Editorial team: Rock deformation, geomorphology, morphotectonics, and paleoseismology | Discipline: Geomorphology
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Oswald Malcles, Philippe Vernant, Jean Chéry, Pierre Camps, Gaël Cazes, Jean-François Ritz, and David Fink
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We aim to better understand the challenging areas that are the intraplate regions using one example: the southern French Massif Central and its numerous hundreds of meters deep valleys. We apply a multidisciplinary approach there using geomorphology, geochronology, and numerical modeling.
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The fall of the Dead Sea level since the 1960s has provoked the formation of over 6000 sinkholes, a major hazard to local economy and infrastructure. In this context, we study the evolution of subsidence phenomena at three area scales at the Dead Sea’s eastern shore from 1967–2017. Our results yield the most detailed insights to date into the spatio-temporal development of sinkholes and larger depressions (uvalas) in an evaporite karst setting and emphasize a link to the falling Dead Sea level.
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Short summary
A 2-D 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 in the Dead Sea region.
A 2-D numerical modelling approach to simulate the mechanical formation of sinkhole cluster...