EGU21-8416
https://doi.org/10.5194/egusphere-egu21-8416
EGU General Assembly 2021
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Calcium-sulfate wedges in the Atacama Desert as indicators for subsurface dynamics

Aline Zinelabedin1, Benedikt Ritter1, Richard Albert2, Dominik Brill3, Axel Gerdes2, Tony Reimann3, Svenja Riedesel3, and Tibor J. Dunai1
Aline Zinelabedin et al.
  • 1Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany (aline.zinelabedin@uni-koeln.de)
  • 2Institute of Geosciences, Goethe-University Frankfurt, Frankfurt, Germany
  • 3Institute of Geography, University of Cologne, Cologne, Germany

Polygonal patterned grounds are common surface expressions of subsurface dynamics in periglacial and Martian environments. In the Periglacial these structures are typically associated with vertically laminated wedges in the subsurface being the product of cryogenic processes. These landscape features similarly occur in arid to hyperarid environments, such as in the Atacama Desert. Due to the salt-dominated soil of the Atacama Desert, haloturbation and salt heave mechanisms control the formation of wedges and polygons under arid conditions. We present x-ray diffraction and x-ray fluorescence analyses of wedges from the central Atacama Desert that contain various calcium-sulfate phases as potential drivers for the wedge-growth activity. The formation of these wedges is connected to varying water activity. Hydration- and dehydration-induced phase transitions of calcium-sulfate phases result in significant volumetric changes in the soils. In combination with crystallisation pressure of (re-)precipitated salts from infiltrated solutions, these processes significantly contribute to the subsurface stress field. The upward stress release is assumed to express in a microtopographic signature of the surface, such as the polygonal patterned ground. In order to investigate the polygon-wedge system under arid conditions, we will present a combination of sedimentological, mineralogical, and geochemical analyses of subsurface wedges from the central Atacama Desert. We also present data constraining the formation age of calcium sulfate-dominated wedges that formed within the El Diablo Formation of Miocene age.

How to cite: Zinelabedin, A., Ritter, B., Albert, R., Brill, D., Gerdes, A., Reimann, T., Riedesel, S., and Dunai, T. J.: Calcium-sulfate wedges in the Atacama Desert as indicators for subsurface dynamics, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-8416, https://doi.org/10.5194/egusphere-egu21-8416, 2021.

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