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Thermal Conductivity Rocks and Soil
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Thermal Conductivity of Soils and Rocks
Typical Apparent Thermal Conductivity Values for Soils, Btu· in/h·ft2 ·°F
Soil | Normal Range |
Recommended Values for Designa |
|
Lowb |
Highc |
||
Sands | 4.2 to 17.4 |
5.4 |
15.6 |
Silts | 6 to 17.4 |
11.4 |
15.6 |
Clays | 6 to 11.4 |
7.8 |
10.8 |
Loams | 6 to 17.4 |
6.6 |
15.6 |
a Reasonable values for use when no site- or soil-specific data are available.
b Moderately conservative values for minimum heat loss through soil (e.g., use in soil
heat exchanger or earth-contact cooling calculations). Values are from Salomone and
Marlowe (1989).
c Moderately conservative values for maximum heat loss through soil (e.g., use in peak
winter heat loss calculations). Values are from Salomone and Marlowe (1989).
Typical Apparent Thermal Conductivity Values for Rocks, Btu· in/h·ft2 ·°F
Rock Composition | Normal Range |
Pumice, tuff, obsidian |
3.6 to 15.6 |
Basalt |
3.6 to 18.0 |
Shale |
6 to 27.6 |
Granite |
12 to 30 |
Limestone, dolomite, marble |
8.4 to 30 |
Quartzose sandstone |
9.6 to 54 |
References
Kersten, M.S. 1949. Thermal properties of soils. University of Minnesota,
Engineering Experiment Station Bulletin 28 (June).
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