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Title:Overview of the thermal properties of rocks and sediments in Slovenia
Authors:ID Rajver, Dušan (Author)
ID Adrinek, Simona (Author)
Files:.pdf PDF - Presentation file, download (6,03 MB)
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Language:English
Typology:1.02 - Review Article
Organization:Logo GeoZS - Geological Survey of Slovenia
Abstract:The use of geothermal energy, which comes from both deep geothermal systems and the shallow underground, has been developing rapidly in the last few decades. The purpose of the paper is to present the results of measurements of the thermal properties of all rock samples and sediments that were available from boreholes, two tunnels and numerous surface locations in Slovenia in the period from 1982 to the end of 2022. In relation to the shallow geothermal potential, a special effort is needed to characterize the thermal properties of the rocks and sediments and to implement thermal energy transfer technology. In this sense, knowledge of the thermal conductivity of rocks and sediments is required to assess the possibility of low-enthalpy heat exchange in a given local area. The largest number of measurements was taken to determine thermal conductivity. Determinations of thermal diffusivity were carried out on a much smaller number of rock and sediment samples, as well as determinations of radiogenic heat production in rocks. The results of thermal conductivity measurements on 430 samples from 119 wells, 20 samples from two tunnels and 156 samples from surface locations are shown. The highest thermal conductivities are shown by samples of dolomite, quartz conglomerate and conglomerate, phyllonite, quartz phyllite and gneiss, while the lowest are measured in sediments such as clay, lignite with clay, peat and dry sand. The determined radioactive heat generation is the lowest for milonitized dolomite and highest for dark grey sandstone with shale clasts. Our results are comparable to those already published worldwide, and they could be the basis for the possible future Slovenian standard for the thermal properties of measured rocks and sediments.
Keywords:thermal conductivity, thermal diffusivity, borehole, tunnel, surface, rock, sediment, radioactive heat generation, Slovenia
Publication status:Published
Publication version:Version of Record
Publication date:04.08.2023
Publisher:Geološki zavod Slovenije
Year of publishing:2023
Number of pages:str. 125-150
Numbering:vol. 66, no. 1
PID:20.500.12556/DiRROS-17639 New window
UDC:550.3
ISSN on article:0016-7789
DOI:10.5474/geologija.2023.005 New window
COBISS.SI-ID:164613891 New window
Publication date in DiRROS:15.01.2024
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Downloads:90
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Record is a part of a journal

Title:Geologija
Shortened title:Geologija
Publisher:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 New window

Document is financed by a project

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0011-2019
Name:Regionalna geologija

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0020-2020
Name:Podzemne vode in geokemija

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Title:Pregled toplotnih lastnosti kamnin in sedimentov v Sloveniji
Abstract:Raba geotermalne energije, ki izhaja iz globokih geotermalnih sistemov kot tudi iz plitvega podzemlja, se v zadnjih nekaj desetletjih hitro razvija. Namen prispevka je prikazati rezultate meritev toplotnih lastnosti vseh vzorcev kamnin in sedimentov, ki so bili na voljo iz vrtin, dveh predorov in številnih površinskih lokacij v Sloveniji v obdobju od 1982 do konca 2022. V zvezi s plitvim geotermalnim potencialom je potrebno posebno prizadevanje za karakterizacijo toplotnih lastnosti tal in plitvega podtalja ter za izvedbo tehnologije prenosa toplotne energije. V tem smislu je potrebno poznavanje toplotne prevodnosti kamnin in tal za oceno možnosti izmenjave toplote z nizko entalpijo na določenem lokalnem območju. Številčno največ meritev je bilo za določitev toplotne prevodnosti. Določitve toplotne difuzivnosti so bile izvedene na precej manjšem številu vzorcev kamnin in sedimentov, prav tako določitve produkcije radiogene toplote v kamninah. Prikazani so rezultati meritev toplotne prevodnosti na 430 vzorcih iz 119 vrtin, na 20 vzorcih iz predorov in na 156 vzorcih iz površinskih lokacij. Najvišje toplotne prevodnosti kažejo vzorci dolomita, kremenovega konglomerata in konglomerata, filonita, kremenovega filita in gnajsa, najniže pa so izmerjene v sedimentih, kot so glina, lignit z glino, šota in suh pesek. Ugotovljena radiogena tvorba toplote je najmanjša pri milonitiziranem dolomitu in največja pri temno sivem peščenjaku s klasti skrilavega glinavca. Naši rezultati so primerljivi z že objavljenimi v svetu in lahko predstavljajo osnovo za morebitni bodoči slovenski standard toplotnih lastnosti merjenih kamnin in sedimentov.
Keywords:toplotna prevodnost, toplotna difuzivnost, vrtina, predor, površje, kamnina, sediment, radiogena tvorba toplote, Slovenija


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