Szczegóły publikacji
Opis bibliograficzny
The quality of geothermal reservoir of the Lower Jurassic aquifer in the Mogilno-Łódź Trough (Polish Lowlands) / Aleksandra Kasztelewicz, Barbara TOMASZEWSKA // E3S Web of Conferences [Dokument elektroniczny]. — Czasopismo elektroniczne ; ISSN 2267-1242. — 2019 — vol. 133 art. no. 02004, s. 1–10. — Wymagania systemowe: Adobe Reader. — Bibliogr. s. 9–10, Abstr. — Publikacja dostępna online od: 2019-11-25. — A. Kasztelewicz - afiliacja: MEERI PAS, Kraków. — AG 2019 : 5th International Conference on Applied Geophysics : Ostrava, Czech Republic : June 27-28, 2019
Autorzy (2)
- Kasztelewicz Aleksandra
- AGHTomaszewska Barbara
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 127160 |
|---|---|
| Data dodania do BaDAP | 2020-01-30 |
| Tekst źródłowy | URL |
| DOI | 10.1051/e3sconf/201913302004 |
| Rok publikacji | 2019 |
| Typ publikacji | referat w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | E3S Web of Conferences |
Abstract
The assessment of the geothermal potential should always take an accurate identification of the geological conditions into account. Petrographic and petrophysical investigations of the aquifers allow to estimate their productivity and infectivity. The area of the Mogilno-ŁódźTrough is next to the Podhale basin, one of the most prospective regions in terms of geothermal potential in Poland. The Lower Jurassic aquifers are characterized by the largest dispositional resources among geothermal aquifers in the Polish Lowlands. The Lower Jurassic geothermal reservoir consist of fine and mixed grain-size sands and sandstones layers from 10-650 m thick, depending on the depth. The water within the reservoir exhibits mineralization ranging from 2 to over 250 g/L and its temperature ranges from 30 to 100°C. Boreholes profiles selected for study consist Lower Jurassic formations of the Polish Lowlands, which are perspective for the heat production in Poland. Sandstones are represent mainly by quartz arenites and subordinate by quartz wackes. Parameters measured include among others porosity, permeability and surface area. The results of the petrographic and mineralogical studies of core samples confirmed the presence of rock with favorable parameters for geothermal water accumulation. © 2019 The Authors, published by EDP Sciences.
