Tests on specimens of reconstituted illitic clay have examined the inf
luence of temperature on the mechanical behaviour of clay soils. The p
rogram involved consolidation to effective confining pressures up to 1
.5 MPa, heating to 100 degrees C, and tests on normally consolidated a
nd overconsolidated specimens with OCR=2. The tests included isotropic
consolidation, undrained triaxial compression with pore water pressur
e measurement, drained tests along controlled stress paths to investig
ate yielding behaviour, and undrained tests which involved heating and
measurement of the resulting induced pore water pressures. The large
strain strength envelope is independent of temperature. However, peak
undrained strengths increase with temperature because smaller pore wat
er pressures are generated during shearing. An important contribution
from the study is a series of results for the yielding of illitic clay
at three different temperatures. For the first time, there is clear e
vidence of yield loci decreasing in size with increasing temperature.
An associated how rule can be assumed without serious error. The resul
ts contribute to the confirmation of a thermal elastic-plastic soil mo
del developed by the authors from cam clay following the addition of a
small number of extra assumptions. Depending on the initial stress st
ate, heating under undrained conditions may produce shear failure. (C)
1997 Elsevier Science B.V.