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Analysis and calculation of thermal conductivity of rock in deep strata
KTH, Skolan för arkitektur och samhällsbyggnad (ABE), Mark- och vattenteknik.
2005 (engelsk)Inngår i: Journal of Central South University of Technology, ISSN 1005-9784, E-ISSN 1993-0666, Vol. 12, s. 114-119Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The thermal conductivity of rock is an important parameter for the deep mine and the geothermal development. It is often not possible to measure the thermal conductivity of the rocks present in the deep strata, and the usual approach is to calculate thermal conductivity including mineralogy and porosity. The compositions of core samples from the MID01 borehole in the Björkö area were determined, and the mineral composition was classified. The calculation of the thermal conductivity of rock in the borehole was carried out, and the main factors for the thermal conductivity of rock were analyzed. The results show that the calculated thermal conductivity of rock is reliable and useful for the design and calculation of geothermal development in the Björkö area.

sted, utgiver, år, opplag, sider
2005. Vol. 12, s. 114-119
Emneord [en]
thermal conductivity of rock, thermal conductivity calculation, mineral composition, rock porosity
HSV kategori
Identifikatorer
URN: urn:nbn:se:kth:diva-37813DOI: 10.1007/s11771-005-0383-4ISI: 000234422700025OAI: oai:DiVA.org:kth-37813DiVA, id: diva2:435335
Merknad
QC 20110818Tilgjengelig fra: 2011-08-18 Laget: 2011-08-17 Sist oppdatert: 2017-12-08bibliografisk kontrollert

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