Heat pulse line-source method to determine thermal conductivity of consolidated rocks
Open Access
- 1 November 1986
- journal article
- Published by AIP Publishing in Review of Scientific Instruments
- Vol. 57 (11) , 2832-2836
- https://doi.org/10.1063/1.1139052
Abstract
An instrument designed to measure thermal conductivity of consolidated rocks, dry or saturated, using a transient method is presented. The instrument measures relative values of the thermal conductivity, and it needs calibration to obtain absolute values. The device can be used as heat pulse line source and as continuous heat line source. Two parameters to determine thermal conductivity are proposed: TMAX, in heat pulse line source, and SLOPE, in continuous heat line source. Its performance is better, and the operation simpler, in heat pulse line-source mode with a measuring time of 170 s and a reproducibility better than 2.5%. The sample preparation is very simple on both modes. The performance has been tested with a set of ten rocks with thermal conductivity values between 1.4 and 5.2 W m−1 K−1 which covers the usual range for consolidated rocks.Keywords
This publication has 5 references indexed in Scilit:
- A transient method and thermophysical parameters of rocks from Dobrudja, northeastern BulgariaTectonophysics, 1984
- Thermal conductivity determinations on solid rock — a comparison between a steady-state divided-bar apparatus and a commercial transient line-source deviceJournal of Volcanology and Geothermal Research, 1984
- The pulse-probe method of conductivity measurementGeophysical Journal International, 1979
- Investigation of a New Simple Transient Method of Thermal Property MeasurementJournal of Heat Transfer, 1974
- The measurement of thermal conductivity of deep-sea sediments by a needle-probe methodJournal of Geophysical Research, 1959