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Journal Article

Beckenmodellierung : Temperatur in Sedimentbecken

Authors
/persons/resource/cacace

Cacace,  Mauro
Vol. 3, Issue 1 (2013), GFZ Journal 2013, System Erde : GFZ Journal, Deutsches GeoForschungsZentrum;
4.4 Basin Analysis, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/leni

Scheck-Wenderoth,  Magdalena
Vol. 3, Issue 1 (2013), GFZ Journal 2013, System Erde : GFZ Journal, Deutsches GeoForschungsZentrum;
4.4 Basin Analysis, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/yvonne

Cherubini,  Yvonne
Vol. 3, Issue 1 (2013), GFZ Journal 2013, System Erde : GFZ Journal, Deutsches GeoForschungsZentrum;
4.4 Basin Analysis, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/przybyci

Przybycin,  Anna Maria
4.4 Basin Analysis, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Fulltext (public)

GFZ_syserde.03.01.09.pdf
(Publisher version), 507KB

Supplementary Material (public)
There is no public supplementary material available
Citation

Cacace, M., Scheck-Wenderoth, M., Cherubini, Y., Przybycin, A. M. (2013): Beckenmodellierung: Temperatur in Sedimentbecken. - System Erde, 3, 1, 62-69.
https://doi.org/10.2312/GFZ.syserde.03.01.9


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_124330
Abstract
The formation of mineral and energy resources involves the interaction of groundwater flow, mechanical deformation, mass and heat transport processes. Thereby, groundwater flow patterns, temperature field, and fluid-rock interactions are all interdependent. This calls for a unified description linking the coupling between the different scales and related physical phenomena involved. A mathematical formulation of the main driving processes affecting basin fluid and heat transport allows developing numerical models as tools to examine the interactions of simultaneously active processes and variable parameters within the constraints given by physical principles and taking into account proper temporal and three dimensional spatial scales. Therefore, the usage of mathematical models is justified by the help they bring in the understanding and verification of specific mechanisms acting in natural systems. In Section “Basin Analysis” at GFZ German Research Centre for Geosciences mathematical models of increasing degree of complexity are applied to the study of energy and mass transport processes in complex sedimentary basins.