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dc.contributor.authorMahmoodpour, Saeed
dc.contributor.authorSingh, Mrityunjay
dc.contributor.authorBär, Kristian
dc.contributor.authorSass, Ingo
dc.date.accessioned2021-11-04T15:19:53Z
dc.date.available2021-11-04T15:19:53Z
dc.date.issued2021-11-04
dc.identifier.urihttps://tudatalib.ulb.tu-darmstadt.de/handle/tudatalib/3099
dc.identifier.urihttps://doi.org/10.48328/tudatalib-671
dc.descriptionHeat production from geothermal reservoirs is controlled by coupled thermo-hydro-mechanical processes and thermal expansion coefficient plays an important role in deciding the fracture aperture. To provide insights on the thermal expansion coefficient values with respect to temperature, two types of sandstones are considered: Remlinger and Flechtinger obtained from Steinbruch, Germany. Measurements are performed with Linseis L75 instrument and the core sample length is 5.26 mm.de_DE
dc.language.isoende_DE
dc.rightsCreative Commons Attribution 4.0
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectHeat and mass transfer in porous mediade_DE
dc.subjectThermal expansion coefficientde_DE
dc.subjectGeothermal reservoirde_DE
dc.subjectThermo-hydro-mechanical simulationsde_DE
dc.subject.classification3.42-01 Geologiede_DE
dc.subject.ddc550
dc.titleDatabase to “Impact of the fracture aperture changes through the fully coupled thermoporoelastic stress on the heat extraction from a fractured reservoir”de_DE
dc.typeDatasetde_DE
tud.projectPTJ | 0324244A | ReSaltde_DE
tud.unitTUDa
tud.history.classificationVersion=2020-2024;314-01 Geologie, Ingenieurgeologie, Paläontologie


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