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Data Publication

3D-CEBS-TTH: transient thermohydraulic model of the Central European Basin System (CEBS)

Frick, Maximilian | Cacace, Mauro | Klemann, Volker | Tarasov, Lev | Scheck-Wenderoth, Magdalena

GFZ Data Services

(2021)

We provide a single file (exodus II format) that contains all results of the modeling efforts of the associated paper. This encompasses all structural information as well as the pore pressure, temperature, and fluid velocity distribution through time. We also supply all files necessary to rerun the simulation, resulting in the aforementioned output file. The model area covers a rectangular area around the Central European Basin System (Maystrenko et al., 2020). The data publication is compeiment to Frick et al., (2021). The file published here is based on the structural model after Maystrenko et al., (2020) which resolves 16 geological units. More details about the structure and how it was derived can be found in Maystrenko et al., (2020). The file presented contains information on the regional variation of the pore pressure, temperature and fluid velocity of the model area in 3D. This information is presented for 364 time steps starting from 43,000 years before present and ending at 310000 years after present. This model was created as part of the ESM project (Advanced Earth System Modelling Capacity; https://www.esm-project.net). This project looks at the development of a flexible framework for the effective coupling of Earth system model components. In this, we focused on the coupling between atmosphere and the subsurface by simulating the response of glacial loading, in terms of thermal and hydraulic forcing, on the hydrodynamics and thermics of the geological subsurface of Central Europe. For this endeavor, we populated the 3D structural model by Maystrenko and Coauthors (2020) with rock physical properties, applied a set of boundary conditions and simulated the transient 3D thermohydraulics of the subsurface. More details about this can be found in the accompanying paper (Frick et al., 2021)

Keywords


Originally assigned keywords
Central Europe
3D Model
Glaciation
subsurface geology
tectonostratigraphic units
formation tops
layer thickness
sedimentary cover
basement rocks
crystalline crust
lithospheric mantle
Northeast German Basin
Central European Basin System
Thermohydraulic Coupling
Nuclear Waste
Transient Process Modelling
Disequilibrium
Climate Change
Paleoclimate
Advanced Earth System Modelling Capacity
ESM
compound material
GLACIER ELEVATIONICE SHEET ELEVATION
GLACIERICE SHEET THICKNESS
GLACIERICE SHEET TOPOGRAPHY
SEDIMENT THICKNESS
GLACIAL LANDFORMSPROCESSES
PALEOCLIMATE
BEDROCK LITHOLOGY
EARTH SCIENCE REANALYSESASSIMILATION MODELS
GEOLOGICTECTONICPALEOCLIMATE MODELS
georeferenced information
sedimentary basin
Phanerozoic
palaeoclimatology
geology
hydrogeology
geophysics
The Present

Corresponding MSL vocabulary keywords
Phanerozoic

MSL enriched keywords
Phanerozoic
Measured property
pore fluid pressure

MSL enriched sub domains i

rock and melt physics


Source publisher

GFZ Data Services


DOI

10.5880/gfz.4.5.2021.003


Authors

Frick, Maximilian

0000-0001-7303-2730

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Cacace, Mauro

0000-0001-6101-9918

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Klemann, Volker

0000-0002-8342-8947

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Tarasov, Lev

Memorial University of Newfoundland;

Scheck-Wenderoth, Magdalena

0000-0003-0426-8269

GFZ German Research Centre for Geosciences, Potsdam, Germany; RWTH Aachen, Aachen, Germany;


Contributers

Frick, Maximilian

ContactPerson

0000-0001-7303-2730

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Frick, Maximilian

ProjectMember

0000-0001-7303-2730

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Frick, Maximilian

Researcher

0000-0001-7303-2730

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Cacace, Mauro

ProjectMember

0000-0001-6101-9918

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Cacace, Mauro

Researcher

0000-0001-6101-9918

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Klemann, Volker

ProjectMember

0000-0002-8342-8947

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Klemann, Volker

Researcher

0000-0002-8342-8947

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Tarasov, Lev

ProjectMember

Memorial University of Newfoundland;

Tarasov, Lev

Researcher

Memorial University of Newfoundland;

Scheck-Wenderoth, Magdalena

ProjectMember

0000-0003-0426-8269

GFZ German Research Centre for Geosciences, Potsdam, Germany; RWTH Aachen, Aachen, Germany;

Scheck-Wenderoth, Magdalena

Researcher

0000-0003-0426-8269

GFZ German Research Centre for Geosciences, Potsdam, Germany; RWTH Aachen, Aachen, Germany;

Maystrenko, Yuri

Researcher

0000-0002-6447-9271

Geological Survey of Norway (NGU), Trondheim, Norway;

Frick, Maximilian

ContactPerson

GFZ German Research Centre for Geosciences, Potsdam, Germany;


References

Cites

Cacace, M., & Jacquey, A. B. (2017). Flexible parallel implicit modelling of coupled thermal–hydraulic–mechanical processes in fractured rocks. Solid Earth, 8(5), 921–941. https://doi.org/10.5194/se-8-921-2017

10.5194/se-8-921-2017

Cites

Frick, M., Scheck-Wenderoth, M., Cacace, M., & Schneider, M. (2019). Boundary condition control on inter-aquifer flow in the subsurface of Berlin (Germany) – new insights from 3-D numerical modelling. Advances in Geosciences, 49, 9–18. https://doi.org/10.5194/adgeo-49-9-2019

10.5194/adgeo-49-9-2019

Cites

Frick, M., Scheck-Wenderoth, M., Schneider, M., & Cacace, M. (2019). Surface to Groundwater Interactions beneath the City of Berlin: Results from 3D Models. Geofluids, 2019, 1–22. https://doi.org/10.1155/2019/4129016

10.1155/2019/4129016

Cites

Kaiser, B. O., Cacace, M., & Scheck-Wenderoth, M. (2013). 3D coupled fluid and heat transport simulations of the Northeast German Basin and their sensitivity to the spatial discretization: different sensitivities for different mechanisms of heat transport. Environmental Earth Sciences, 70(8), 3643–3659. https://doi.org/10.1007/s12665-013-2249-7

10.1007/s12665-013-2249-7

Cites

Koltzer, N., Scheck-Wenderoth, M., Bott, J., Cacace, M., Frick, M., Sass, I., Fritsche, J.-G., & Bär, K. (2019). The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany). Energies, 12(11), 2081. https://doi.org/10.3390/en12112081

10.3390/en12112081

Cites

Maystrenko, Y. P., Scheck-Wenderoth, M., &amp; Anikiev, D. (2020). <i>3D-CEBS: Three-dimensional lithospheric-scale structural model of the Central European Basin System and adjacent areas</i> (Version 1). GFZ Data Services. https://doi.org/10.5880/GFZ.4.5.2020.006

10.5880/GFZ.4.5.2020.006

Cites

Tarasov, L., Dyke, A. S., Neal, R. M., & Peltier, W. R. (2012). A data-calibrated distribution of deglacial chronologies for the North American ice complex from glaciological modeling. Earth and Planetary Science Letters, 315–316, 30–40. https://doi.org/10.1016/j.epsl.2011.09.010

10.1016/j.epsl.2011.09.010

Cites

Tarasov, L., & Richard Peltier, W. (2002). Greenland glacial history and local geodynamic consequences. Geophysical Journal International, 150(1), 198–229. https://doi.org/10.1046/j.1365-246x.2002.01702.x

10.1046/j.1365-246X.2002.01702.x

IsDerivedFrom

Frick, M., Cacace, M., Klemann, V., Tarasov, L., & Scheck-Wenderoth, M. (2022). Hydrogeologic and Thermal Effects of Glaciations on the Intracontinental Basins in Central and Northern Europe. Frontiers in Water, 4. https://doi.org/10.3389/frwa.2022.818469

10.3389/frwa.2022.818469

IsSupplementTo

References


Contact

Frick, Maximilian

GFZ German Research Centre for Geosciences, Potsdam, Germany;

Frick, Maximilian

GFZ German Research Centre for Geosciences, Potsdam, Germany;


Citiation

Frick, M., Cacace, M., Klemann, V., Tarasov, L., & Scheck-Wenderoth, M. (2021). 3D-CEBS-TTH: transient thermohydraulic model of the Central European Basin System (CEBS) [Data set]. GFZ Data Services. https://doi.org/10.5880/GFZ.4.5.2021.003


Geo location(s)

temporal coverage: 43,000 years before present 310,000 years after present