MMIJ 2025, Sapporo

Presentation information (2025/08/07 Ver.)

General Session

(General session) Rock Engineering / Mining technologies

Tue. Sep 2, 2025 1:00 PM - 4:50 PM Room-1(212, 2Fl, C Block)

Chairperson: 奈良禎太(京都大学)、才ノ木敦士(熊本大学)、吉光奈奈(京都大学)

●岩盤工学:岩盤の力学特性,地山応力など、地下の岩盤の状態の把握に必要な基礎的な試験技術,解析技術、そしてこうした技術を用いたケーススタディについて議論を行う。

●資源開発技術:エネルギーや金属鉱物などの資源の開発に必要な上流から下流までの開発・生産の技術に関する科学的・技術的な現状および課題について議論を行う

(Presentation: 15 minutes allotted for lecture and 5 minutes for Q&A out of 20 minutes per presentation)

2:35 PM - 2:55 PM

[1110-19-05] Development and Validation of a Custom Divided-Bar Apparatus for Accurate Thermal Conductivity Measurements in Rock Core Samples

○Prasad Chathurangana Karunarathne1[Student presentation: Doctoral course], Weiren Lin1 (1. Department of Urban Management, Kyoto University)

司会:才ノ木敦士(熊本大学)

Keywords:Rock cores, Thermal properties, Steady state measurement, Laboratory model

Rocks interact with heat in complex ways, influenced by their formation, deformation, and hydrothermal processes. Classified as igneous, sedimentary, or metamorphic, rocks undergo chemical and physical changes due to temperature, pressure, and fluids, with temperature being the dominant factor. Their thermal behavior is crucial for applications like geothermal energy, radioactive waste disposal, and deformation studies, necessitating precise measurement of thermophysical properties such as thermal conductivity (TC), diffusivity, and heat capacity. Laboratory methods for measuring TC include steady-state (e.g., divided-bar) and transient techniques. This study used a custom divided-bar apparatus with continuous temperature monitoring. A major limitation is heat loss (40–50%) from the vertical Sample assembly, traditionally mitigated by calibration with standard samples. The thermal conductivity of Sharma sandstone core samples was measured and subsequently validated against established reference values to assess potential limitations in the custom-designed experimental setup.

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