An electron-diffraction study of the structure of silver films condensed in vacuo on rocksalt cleavage faces at about 200° c., and of the changes produced by heating these films in vacuo, has shown that the reflection and transmission patterns are in general agreement with Menzer's view of the twinned structure of such films. The films examined yielded patterns of a type indicating strong {111} extensions of the reciprocal-lattice intensity regions, but without marked development of [001] extensions. No conclusive evidence has been found of development of octahedral boundary faces of the films in addition to the twinning which occurs on these planes.
The positions of the diffraction spots and lines in patterns from films which had become distorted during the dissolution of the substrate and the mounting of the film showed that parts of the film had become considerably curved about axes parallel to the cube axes and cube-face diagonal directions in the film plane. These types of curvature are in agreement with the form of the substrate surface and the twinned structure of the films. General equations are derived for use in considering the geometrical features of rotation patterns yielded by cubic crystals.
Heating in vacuo at about 500° c. quickly converts the silver films into normal relatively perfect single crystals in the same orientation as that part of the initial film whose lattice was parallel to that of the rocksalt substrate. Such an extensive atomic rearrangement testifies to a high mobility of the silver atoms at temperatures much below the melting point; this has been inferred by previous investigators, but in this case is shown to occur within the lattice and not merely on its surface.