WHITE CAST IRON
White
cast iron displays white fractured surfaces due to the presence of an iron
carbide precipitate called cementite. With a lower silicon content
(graphitizing agent) and faster cooling rate, the carbon in white cast iron
precipitates out of the melt as the metastable phase cementite, Fe3C, rather than
graphite. The cementite which precipitates from the melt forms as relatively
large particles. As the iron carbide precipitates out, it withdraws carbon from
the original melt, moving the mixture toward one that is closer to eutectic,
and the remaining phase is the lower iron-carbon austenite (which on cooling might
transform to martensite). These eutectic carbides are
much too large to provide the benefit of what is called precipitation hardening
(as in some steels, where much smaller cementite precipitates might inhibit plastic deformation by
impeding the movement of dislocations through the pure iron ferrite
matrix). Rather, they increase the bulk hardness of the cast iron simply by
virtue of their own very high hardness and their substantial volume fraction,
such that the bulk hardness can be approximated by a rule of mixtures. In any
case, they offer hardness at the expense of toughness. Since carbide makes up a large
fraction of the material, white cast iron could reasonably be classified as a cermet. White iron is too brittle for
use in many structural components, but with good hardness and abrasion
resistance and relatively low cost, it finds use in such applications as the
wear surfaces (impeller and volute) of slurry pumps, shell liners and lifter bars in ball mills and autogenous
grinding mills, balls and rings in coal pulverisers, and the teeth of a backhoe's digging bucket (although cast
medium-carbon martensitic steel is more common for this application).
Nominal
composition [% by weight] :
C 3.4, Si 0.7, Mn 0.6
Tensile strength
[ksi] : 25
Hardness [Brinell
scale] : 450
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