The authors describe the tests which were carried out in order to explain the relation between the process of nucleation and growth and the crystal structucture of graphites in various cast irons. Flake graphite, spheroidal one and temper carbon were prepared from gray iron, OZ-ductile iron and malleable cast iron by electrolytic extraction. The crystal structures of graphites and carbon were determined by X-ray diffraction. The results obtained are as follows: 1) The values of the spacing, the lattice constant and the C-C distance determined illustrated that all the specimens had a crystal structure for the typical grapite. 2) The diffraction lines of the flake and the spheroidal graphites were very sharp, but the lines of the temper carbon were broad compared with the other two lines. Also, the latter (100) and (101) line profiles were more asymmetrical than the former line profiles. 3) The values of Lc (001) of the flake graphite were all above 1,000 A only at the lower scattering angle side but at the higher scattering angle they became smaller. This tendency of the spheroidal graphite and the temper carbon would be caused by the strain of crystal lattices. The La (110) values of each specimens were above 1,000 A. 4) The strain of crystal lattice is given by
β(obs)•cos
θ=
η •sin
θ+K •
λ/D, ············(1) where
β(obs) is the observed half maximum line breadth,
θ the scattering angle,
η the parameter of lattice strain, K the shape factor,
λ the wavelength and D the crystallite size. The results are shown in Fig. 1. As shown in Fig. 1, the strain of crystal lattices was the largest in temper carbon, being slightly smaller in spheroidal graphite and almost nothing in flake graphite. 5) The difference in graphite crystal structures may possibly depend not only upon the nucleation, growth condition and shape of crystals, but the internal stresses of the matrix caused during the solidification.
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