Abstract
The residual lattice strains in three types of aluminium have been measured using X-ray diffraction methods and have been compared quantitatively with the theory of an intergranular stress system postulated by G.B. Greenough [1]. A discrepancy between theory and experiment has been observed with specimens in the form of tensile test pieces. It is concluded that these results raise doubts as to the validity of the theory in its present form.
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