Thermal properties of soils are of great importance in view of the subsurfa
ce transmission of either heated fluids or high power currents. For these s
ituations, it is essential to estimate the resistance offered by the soil m
ass in dissipating the heat generated through it. Thermal resistivity of so
ils is a complex phenomenon that depends upon various parameters, viz., typ
e of the soil, particle size distribution, its compaction characteristics,
etc. A laboratory probe has been developed based upon the principle of tran
sient method to measure thermal resistivity of different soils for a state
of compaction. Based on these results, generalised relationships have been
developed, for predicting soil thermal resistivity, and their efficiency ha
s been established by comparing the obtained results with those available i
n literature. (C) 2000 Elsevier Science Inc. All rights reserved.