Three thermal probes were constructed in accordance with ASTM D 5334 and ca
librated using heat-flow metre data. The temperature-time response of the t
hermal probes for determining apparent thermal conductivity lambda under tr
ansient state conditions was logged at 1 s intervals. The instrumentation u
sed reduced the determinate error associated with voltage and current measu
rements to a negligibly small value that made the uncertainty in lambda dep
endent on the uncertainty of the slope dT/dlnt. A test method was run in 10
00 s, in which a criterion of 2.5% spread among three consecutive slope val
ues was used to determine the extent of the linear segment of the T-ln t cu
rve.
The probes demonstrated repeatability within +/- 3.5% but had definite indi
vidual bias indicating a need for individual calibration. Using individual
probe calibration factors, the experimentally determined lambda s for all-p
urpose sand, sifted sand, and soil were determined to be 0.520, 0.445, and
2.11 W/m.K, respectively.