| Autor: |
Schärli, Ulrich, Rybach, Ladislaus |
| Zdroj: |
Tectonophysics; January 1984, Vol. 103 Issue: 1 p307-313, 7p |
| Abstrakt: |
Measurements by a Quick Thermal Conductivity Meter on dry and water-saturated granitic samples at room temperature are reported. For a porosity of 0.8% the difference between dry and water-saturated conductivities amounts to 30%. The measured conductivities are in good agreement with values calculated for a pore configuration model based on interconnected crack-type pores. Rapid thermal conductivity measurements on dry and water-saturated samples have a considerable potential as a method to determine porosity in low-porosity crystalline rocks. |
| Databáze: |
Supplemental Index |
| Externí odkaz: |
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