Details

Reconstructing rock temperature profiles from field measurements using finite element modelling and inverse analysis
ID Dujc, Jaka (Author)

.pdfPDF - Presentation file, Download (402,36 KB)
MD5: 0B9BC435D9023B825384C7B25352CEE1
URLURL - Source URL, Visit https://www.matec-conferences.org/articles/matecconf/abs/2026/04/matecconf_engopt2026_03011/matecconf_engopt2026_03011.html This link opens in a new window

Abstract
Rock temperature evolution plays a key role in the development of freeze-thaw cycles that contribute to progressive rock damage and rockfall formation. Understanding the spatial and temporal distribution of temperature inside rock masses is therefore essential for studying thermally induced degradation processes in natural rock slopes. However, in situ measurements typically provide temperature data only at a few discrete depths, which makes it difficult to determine the complete temperature field within the rock. This study presents a computational framework that combines field measurements, finite element simulations and optimisation techniques to reconstruct the temperature distribution inside rock formations. Heat transfer in the rock mass is modelled using a one-dimensional transient heat conduction model based on the finite element method. The reconstruction of the temperature field is formulated as a sequential optimisation problem. In the first step, the thermal diffusivity of the rock is determined by minimising the discrepancy between measured and simulated temperatures. In the second step, the unknown temperature boundary condition at the rock surface is identified using an optimisation procedure. The optimised parameters are then used in a final simulation to compute the continuous temperature profile throughout the rock depth. The methodology is applied to a monitored rock face in eastern Slovenia and produces a stable and physically consistent temperature field. The reconstructed temperature field reveals the propagation of temperature variations into the rock mass and allows the identification of depths and time periods where the temperature drops below freezing.

Language:English
Work type:Article
Typology:1.08 - Published Scientific Conference Contribution
Organization:FGG - Faculty of Civil and Geodetic Engineering
Publication status:Published
Publication version:Version of Record
Year:2026
Number of pages:9 str.
Numbering:Vol. 422, art. 03011
PID:20.500.12556/RUL-188479 This link opens in a new window
UDC:519.62
ISSN on article:2261-236X
DOI:10.1051/matecconf/202642203011 This link opens in a new window
COBISS.SI-ID:292126723 This link opens in a new window
Publication date in RUL:23.09.2026
Views:41
Downloads:10
Metadata:XML DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Record is a part of a proceedings

Title:EngOpt 2026
COBISS.SI-ID:292124163 This link opens in a new window

Record is a part of a journal

Title:MATEC web of conferences
Shortened title:MATEC web conf.
Publisher:EDP Sciences-Web of conferences
ISSN:2261-236X
COBISS.SI-ID:524597785 This link opens in a new window

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
Keywords:metoda končnih elementov, inverzna analiza, rekonstrukcija temperaturnega profila, spremljanje temperature kamnine, cikli zmrzovanja, cikli tajanja

Projects

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:J1-3024
Name:Dešifriranje občutljivosti skalnih sten na podnebne spremembe in cikle zmrzovanja in odtaljevanja na območjih brez permafrosta

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P2-0210
Name:E-Gradbeništvo

Similar documents

Similar works from RUL:
Similar works from other Slovenian collections:

Back