Accurate evaluation of sigma(mu), the internal stress, is essential fo
r determining sigma, the effective stress, because experimental yield
stress data yield only the sum of sigma and sigma(mu). In the past,
the most popular method of determining sigma(mu) has been the back ext
rapolation technique which assumes that sigma = 0 at the now stress p
lateau of a constant strain rate sigma vs. T plot, so that in this reg
ion sigma = sigma(mu). Back extrapolating this cr, to absolute zero wh
ile giving it the temperature dependence of the shear modulus was then
assumed to determine sigma(mu) at temperatures below the plateau. Thi
s technique has been shown to seriously overestimate sigma(mu) and und
erestimate sigma and it has been shown that sigma(mu) may be measured
more accurately [1,2,3] using strain rate sensitivity data. However,
strain rate sensitivity data at sub-ambient temperatures are very diff
icult to obtain accurately. This paper discusses another possible meth
od for measuring sigma(mu) based on Hall-Fetch data, which appears to
be much easier to use and of still greater accuracy.