2016
DOI: 10.1016/j.renene.2016.07.028
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The Podhale geothermal reservoir simulation for long-term sustainable production

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Cited by 44 publications
(22 citation statements)
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“…In Poland, the absolute value of water temperature is determined with the surface changes in intensity of the normal heat flow of the Earth. The value of the heat flow ranges from 25-40 mW/m 2 in the Precambrian platform up to 50-90 mW/m 2 within the Palaeozoic platform and 50-80 mW/m 2 in the Alps orogen of the Carpathians (Bujakowski et al 2016). For Podhale, the density of the heat flow is estimated at 60-70 mW/m 2 and differs slightly from the average world density of geothermal energy stream of 60 mW/m 2 (Sobański et al 2000).…”
Section: Methods Of Geothermal Step Calculationmentioning
confidence: 99%
“…In Poland, the absolute value of water temperature is determined with the surface changes in intensity of the normal heat flow of the Earth. The value of the heat flow ranges from 25-40 mW/m 2 in the Precambrian platform up to 50-90 mW/m 2 within the Palaeozoic platform and 50-80 mW/m 2 in the Alps orogen of the Carpathians (Bujakowski et al 2016). For Podhale, the density of the heat flow is estimated at 60-70 mW/m 2 and differs slightly from the average world density of geothermal energy stream of 60 mW/m 2 (Sobański et al 2000).…”
Section: Methods Of Geothermal Step Calculationmentioning
confidence: 99%
“…Geological conditions of geothermal resources in Poland have been analyzed since the 80s of last century and geothermal waters have already found applications in heating, balneotherapy and recreation [8][9][10][11]. Those geothermal resources are related to underground waters of different stratigraphic layers (thereby various depths) within four major provinces that are subsequently: the Polish Lowlands, the Carpathians, the Carpathian Foredeep and the Sudetes (Fig.…”
Section: Geothermal Energy Resources In Polandmentioning
confidence: 99%
“…Investigated geothermal water is classified as sulfate-chloride-sodium-calcium water (according to Szczukariew-Prikłoński classification). Mineralization of these waters is about 2.5 g/L, including specific component such as a metasilicic acid [5][6][7][8] and a temperature is between 82.9-86.3°C [9].…”
Section: Characteristic Of the Research Areamentioning
confidence: 99%