#

Analysing reservoir properties of the Liassic sedimentary layer in Poland

Skoða fulla færslu

Titill: Analysing reservoir properties of the Liassic sedimentary layer in PolandAnalysing reservoir properties of the Liassic sedimentary layer in Poland
Höfundur: Kurowska, Ewa ; Jarðhitaskóli Háskóla Sameinuðu þjóðanna
URI: http://hdl.handle.net/10802/23478
Útgefandi: United Nations University; Orkustofnun
Útgáfa: 2000
Ritröð: United Nations University., UNU Geothermal Training Programme, Iceland. Report ; 2000:11
Efnisorð: Jarðhiti; Jarðhitarannsóknir; Jarðhitasvæði; Setlög; Pólland
ISSN: 1670-7427
Tungumál: Enska
Tengd vefsíðuslóð: http://www.os.is/gogn/unu-gtp-report/UNU-GTP-2000-11.pdf
Tegund: Bók
Gegnir ID: 001516449
Athugasemdir: Myndefni: kort, línurit, töflur.
Útdráttur: 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.


Skrár

Skrá Stærð Skráartegund Skoða Lýsing
UNU-GTP-2000-11.pdf 935.8Kb PDF Skoða/Opna Heildartexti

Þetta verk birtist í eftirfarandi flokki:

Skoða fulla færslu

Leita


Fletta