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Titill:
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Analysing reservoir properties of the Liassic sedimentary layer in PolandAnalysing reservoir properties of the Liassic sedimentary layer in Poland |
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Höfundur:
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Kurowska, Ewa
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Jarðhitaskóli Háskóla Sameinuðu þjóðanna
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URI:
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http://hdl.handle.net/10802/23478
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Útgefandi:
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United Nations University; Orkustofnun
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Útgáfa:
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2000 |
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Ritröð:
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United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 2000:11 |
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Efnisorð:
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Jarðhiti; Jarðhitarannsóknir; Jarðhitasvæði; Setlög; Pólland
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ISSN:
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1670-7427 |
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Tungumál:
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Enska
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Tengd vefsíðuslóð:
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http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2000-11.pdf
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Tegund:
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Bók |
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Gegnir ID:
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991010426329706886
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Athugasemdir:
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Myndefni: kort, línurit, töflur. |
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Útdráttur:
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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. |
