Stationary reverse temperature modelling and geothermal resources callibration for the Košice Depression (Eastern Slovakia)

Jacko, S.; Fričovský, B.; Pachocka, K.; Vranovska, A.

Artykuł - szczegóły

Tytuł artykułu

Stationary reverse temperature modelling and geothermal resources callibration for the Košice Depression (Eastern Slovakia)

Autorzy

Jacko S. , Fričovský B. , Pachocka K. , Vranovska A.

Treść / Zawartość

Pełne teksty:

tpg_2014_1_Jacko_i_in-stationary-reverce.pdf

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Warianty tytułu

Odwrotne modelowanie warunków termicznych oraz kalibracja zasobów geotermalnych dla Depresji Koszyc (Wschodnia Słowacja)

Języki publikacji

Abstrakty

The south-eastern part of the Košice Depression contains prospective accumulations of geothermal waters having a discharge temperature of 123–129°C at exploration wells. Clastic rocks of the Neogene formation base (Carpathian) and Triassic dolomites of the Čierna hora Mts. Veporic basement form geothermal water aquifers. Using PETREL software for re-evaluation of seismic sounding results and drilled wells data it was possible to make a more accurate determination of the geological boundaries’ spatial positions, and to create a 3D model of the area delimiting four lithologically and stratigraphically different bodies at the most promising locality (i.e. the Ďurkov village area). Heat flowmodelling calculated the geothermal gradient for each aquifer body, e.g. Sarmatian (G_tr »38.1–60.6°C/km), Badenian (G_tr »41–56.1°C/km), Carpathian (G_tr »38.3–51.4°C/km), and Mesozoic (G_tr »22.4–30.6°C/km). Depth temperature distribution fluctuated between 36°C and 138°C on average (from 500 to 3000 m beneath the surface).

W południowo-wschodniej części Depresji Koszyc występują złoża wód geotermalnych o temperaturze na wypływie 123–129°C. Zbiorniki tych wód budują skały klastyczne formacji neogeńskiej (karpatu) oraz dolomity triasowe gór Čiernej hory należące do podłoża weporskiego. Do ponownej oceny wyników badań sejsmicznych oraz badań otworowych wykorzystano oprogramowanie PETREL, co pozwoliło na dokładniejsze przestrzenne określenie granic geologicznych oraz na opracowanie modelu 3D obszaru ograniczonego czterema różnymi pod względem litologicznym i stratygraficznym ośrodkami skalnymi w najbardziej perspektywicznym obszarze miejscowości Ďurkov. W ramach omawianych w artykule prac wykonano modelowanie przepływu ciepła oraz obliczono gradient geotermalny dla każdego ze zbiorników wód, tj.: sarmackiego (G_tr» 38,1–60,6°C/km), badeńskiego (G_tr» 41–56,1°C/km), karpackiego (G_tr» 38,3–51,4°C/km) oraz mezozoicznego (G_tr» 22,4–30,6°C/km). Temperatury na głębokościach od 500 do 3000 m p.p.t. zmieniają się w zakresie od 36 do 138°C.

Słowa kluczowe

Durkov Košice Depression geothermal resources reserves resources temperature modelling

Durkov wieś depresja Koszyc zasoby geotermalne zasoby eksploatacyjne modelowanie temperatur

Wydawca

Instytut Gospodarki Surowcami Mineralnymi i Energią PAN

Czasopismo

Technika Poszukiwań Geologicznych

Rocznik

2014

Tom

R. 53, nr 1

Strony

3--25

Opis fizyczny

Bibliogr. 46 poz., rys., tab., wykr.

Twórcy

autor

Jacko S.

stanislav.jacko@tuke.sk.

Institute of Geosciences, Faculty of Mining, Ecology, Process Control and Geotechnologies, Technical University of Košice, Slovak Republic

autor

Fričovský B.

branislav.fricovsky@tuke.sk

Institute of Geosciences, Faculty of Mining, Ecology, Process Control and Geotechnologies, Technical University of Košice, Slovak Republic

autor

Pachocka K.

katarina.pachocka@tuke.sk

Institute of Geosciences, Faculty of Mining, Ecology, Process Control and Geotechnologies, Technical University of Košice, Slovak Republic

autor

Vranovska A.

vranovska@vuvh.sk

Water Research Institute, Nábrežie arm. gen. L. Svobodu 5, 812 49 Bratislava, Slovak Republic

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