Articles | Volume 9, issue 6
https://doi.org/10.5194/se-9-1341-2018
© Author(s) 2018. 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-9-1341-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Geomechanical modelling of sinkhole development using distinct elements: model verification for a single void space and application to the Dead Sea area
Djamil Al-Halbouni
CORRESPONDING AUTHOR
Helmholtz Centre – German Research Centre for Geosciences (GFZ),
Section 2.1, Telegrafenberg, Potsdam, 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, Australia
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),
Section 2.1, Telegrafenberg, Potsdam, Germany
Institute of Earth and Environment, University of Potsdam, Potsdam, Germany
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Djamil Al-Halbouni, Robert A. Watson, Eoghan P. Holohan, Rena Meyer, Ulrich Polom, Fernando M. Dos Santos, Xavier Comas, Hussam Alrshdan, Charlotte M. Krawczyk, and Torsten Dahm
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The rapid decline of the Dead Sea level since the 1960s has provoked a dynamic reaction from the coastal groundwater system, with physical and chemical erosion creating subsurface voids and conduits. By combining remote sensing, geophysical methods, and numerical modelling at the Dead Sea’s eastern shore, we link groundwater flow patterns to the formation of surface stream channels, sinkholes and uvalas. Better understanding of this karst system will improve regional hazard assessment.
Robert A. Watson, Eoghan P. Holohan, Djamil Al-Halbouni, Leila Saberi, Ali Sawarieh, Damien Closson, Hussam Alrshdan, Najib Abou Karaki, Christian Siebert, Thomas R. Walter, and Torsten Dahm
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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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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
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Subject area: The evolving Earth surface | Editorial team: Rock deformation, geomorphology, morphotectonics, and paleoseismology | Discipline: Mineral and rock physics
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Short summary
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.
Sinkholes are round depression features in the ground that can cause high economic and life...