2015
DOI: 10.1016/j.renene.2015.02.018
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Modelling geothermal and operating parameters of EGS installations in the lower triassic sedimentary formations of the central Poland area

Abstract: a b s t r a c tThe article presents the results of modelling geothermal conditions in the Lower Triassic sedimentary formations of the Polish Lowland area (central Poland) and an electricity production model for a prospective EGS (Enhanced Geothermal System) installation situated in that area. On the basis of comprehensive analyses, this area has been selected as optimal for EGS plants operating in sedimentary complexes in the Polish Lowland. Numerical modelling was conducted using TOUGH2 code and served to ev… Show more

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Cited by 48 publications
(17 citation statements)
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“…The simulation experimentation results show that the thermal conductivity is the most influencing parameter regarding the production temperature because of its direct relationship with permeability, as confirmed by experimental studies; as the permeability increases, the thermal conductivity rises [36]. The simulation also indicates that porosity has the least effect concerning the reservoir's productivity, compared to the other parameters.…”
Section: Parametersupporting
confidence: 55%
“…The simulation experimentation results show that the thermal conductivity is the most influencing parameter regarding the production temperature because of its direct relationship with permeability, as confirmed by experimental studies; as the permeability increases, the thermal conductivity rises [36]. The simulation also indicates that porosity has the least effect concerning the reservoir's productivity, compared to the other parameters.…”
Section: Parametersupporting
confidence: 55%
“…Numerical modelling was conducted using TOUGH2 code (Bujakowski et al, 2015). The modelled net power of an EGS plant operating in the Kutno area ranged from 1.3 to 1.6 MW depending on the permeability and volume of the fractured zone used for the circulation (Bujakowski et al, 2015). In the Konin area net power of an EGS plant was estimated to range from 1.9 to 2.2 MW, while in in the Pleszów area EGS plant net power was assessed at 2.2-2.5 MW (Wójcicki et al, 2013).…”
Section: Analysis Of the Resultsmentioning
confidence: 99%
“…Geothermal energy resources in Poland are related to the underground waters of different stratigraphic layers occurring at different depths, within geological units in the Polish Lowland, the Sudetes and the Carpathians. The information about their size is widely known thorough results of numerous research projects [12][13][14][15][16][17][18][19]. The recognition of geological structures for direct or indirect applications of the geothermal energy is an important direction of carried geological research.…”
Section: Geothermal Energy In Polandmentioning
confidence: 99%