This is a malleable cast iron after conversion to nodular
graphite, shown at 100X. The silicon content and size of the casting (i.e., the section thickness) were both kept sufficiently low that the nucleation of graphite was suppressed during solidification. The casting froze as a mixture of cementite plus austenite called white cast iron (from its characteristic fracture appearance, compared to graphitic grey cast iron). The room temperature microconstituent formed from the eutectic austenite plus iron carbide is called ledeburite, which is usually pearlite plus massive cementite. Upon prolonged heating at up to 930C over a period of several days, the cementite decomposes to austenite plus spheroidal graphite. During subsequent slow cooling to room temperature, the austenite decomposes to ferrite plus additional graphite. The silicon content is critical; too much causes graphite formation during freezing; too little prolongs the solid state graphitization process. About 1% silicon is best. |
Here are a few of the irregularly shaped graphite nodules at
500X, shown with the contrast reduced to aid
the visualization of the relatively unreflective graphite. This microstructure is far more ductile than grey (i.e., flake graphite) cast iron, because these graphite nodules have rounded edges in spite of their lumpy appearance, compared to the very sharp edges of the disk-shaped graphite flakes in grey cast iron. |