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Analysing reservoir properties of the Liassic sedimentary layer in Poland

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dc.contributor Jarðhitaskóli Háskóla Sameinuðu þjóðanna is
dc.contributor.author Kurowska, Ewa is
dc.date.accessioned 2020-06-25T14:35:08Z
dc.date.available 2020-06-25T14:35:08Z
dc.date.issued 2000
dc.identifier.issn 1670-7427
dc.identifier.uri http://hdl.handle.net/10802/23478
dc.description Myndefni: kort, línurit, töflur. is
dc.description.abstract Geothermal water is used in a few places in Poland, mainly for space heating, balneology, bathing, greenhouse cultivation and fish farming. Two operating geothermal plants show good prospects for the future in low-enthalpy geothermal water utilisation, and also new plants being designed. In this paper geothermal resources within the Polish sedimentary basin, covering 80% of Poland's area, are presented. The analysis of temperature and heat flow distribution in Poland, and also of the Early Jurassic (Liassic) water-bearing layer was performed to show the main reservoir features. The Liassic sandstone reservoir includes geothermal water up to 120°C at depths of 3800 m, and together with Early Cretaceous formations has the highest geothermal potential and the best conditions for geothermal water extraction and utilization in Poland. is
dc.format.extent 1 rafrænt gagn (14 bls.) is
dc.language.iso en
dc.publisher United Nations University is
dc.publisher Orkustofnun is
dc.relation.ispartofseries United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 2000:11
dc.relation.uri http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2000-11.pdf
dc.subject Jarðhiti is
dc.subject Jarðhitarannsóknir is
dc.subject Jarðhitasvæði is
dc.subject Setlög is
dc.subject Pólland is
dc.title Analysing reservoir properties of the Liassic sedimentary layer in Poland en
dc.title.alternative Geothermal training in Iceland en
dc.type Bók is
dc.identifier.gegnir 991010426329706886


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