article · E3S Web of Conferences
This work focuses on studying the impact of porosity and fluid saturation on the thermal conductivity of calcarenite rocks. The porosity of these porous materials is measured using the water porosity technique, and thermal conductivity is measured using thermal conductivity scanning (TCS). Models for predicting the thermal properties of rocks have been established. The results obtained show that thermal conductivity values increase considerably in the saturated state compared to the dry state. Comparison of the experimental results and theoretical predictions shows that the thermal conductivity values lie between the two theoretical limits, with values closer to the parallel model, indicating that water saturation promotes heat transfer through the solid matrix.
This page summarises published work. The authoritative version sits with the publisher.
DOI: 10.1051/e3sconf/202568000140
Is something wrong with this record? Report it or request removal.
Discussion
Have you built on this work, tried to replicate it, or seen it applied in practice? Share what you know. Verified researchers and MARATTO™ domain experts can open a discussion, and any member can reply. Contributions are reviewed before they appear.
No discussion yet. Open the first thread.
New to MARATTO™? Create a free account.