Three predictive models are tested against soil thermal conductivity data a
t high temperatures: two (deV-1 and deV-2) are modifications of the origina
l de Vries model, and the third is the Gori model. Model deV-1 results corr
elated very closely for 30, 50 and 70 degrees C, and moderately close for 9
0 degrees C. Generally, this model does not require the use of a mass trans
fer enhancement factor. The Gori model results correlated well at 30 and 50
degrees C. Model deV-2 results correlate well above field capacity, and pr
ovide the best predictions at full dryness. Model deV-1 is recommended for
computer modelling of heat and moisture movement in soils at high temperatu
res. Copyright (C) 2000 John Wiley & Sons, Ltd.