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The
Production of Crucible steel and the Damascus Pattern There are two fundamental factors that will
profoundly influence the final characteristics of the steel product: the
crucible charge and the forging method.
The materials and methods used to produce and forge the ingot will directly
affect whether or not a pattern can be produced. Modern replication experiments,
historical and ethnographic accounts demonstrate that there are many possible
ingredients that can be used for the crucible charge to produce a crucible steel
ingot. They have also determined
particular factors which are necessary to produce a pattern.
Al-Beruni
stated that farand (the Damascus pattern) was not the result of
industry and design, but was an accidental product (Said, 1989, 218). Curiously,
Wilkinson (1937, 193) made a similar statement a thousand years later, “…the
figure of the genuine ancient and modern Damascus sword-blades is the result of
nature, and not of art”. More
recent research by various scholars has determined the factors which affect the
formation of the pattern and it is now known that the pattern is indeed the
result of the nature of steel, although a certain amount of “art and
industry” of forging is also required. Essentially
crucible steel can be produced from an infinite number of possible crucible
charge ingredients containing iron and carbon. The presence of minor and trace
elements in the crucible charge, via the source of iron, carbon or additional
substances added to the charge, will also affect the steel ingot. These elements
can affect the forging of the ingot (e.g. in rendering it “hot short” due to
phosphorus) in addition to the performance and appearance of the final product. The
percentage of the carbon content of the crucible steel is significant for the
creation of different types of patterns and the performance of the blade.
Hypoeutectoid (< 0.8% C) and hypereutectoid (> 0.8% C) steel can produce a
pattern, but the microstructure and, therefore, the pattern will be noticeably
different. Hypoeutectoid steel will produce a banded pattern (e.g. Sham
pattern), however, the most characteristic Damascus steel patterns (e.g. Kara
Khorasan pattern) is produced from hypereutectoid steel. Hypoeutectoid
ingots produce ferrite-pearlite banding. A factor in the production of the
banding is the presence of elements, which during the solidification of the
liquid ingot, remain in the interdendritic region
(Samuels, 1980, 129). Pearlite will form in the interdendritic band,
possibly influenced by the presence of manganese. According to Samuels (1980,
129) the dendrite itself is composed primarily of ferrite and very slow cooling
will produce bigger bands. Studies,
primarily lead by Verhoeven (e.g. 2001) have found that the formation of
the pattern in hypereutectoid steels is due to the alignment of
globular/spherical cementite in the interdendritic zones. The cementite aligns
because of the presence of impurity elements present in the interdendritic zone.
Verhoeven et al. (1998) determined that elements
such as vanadium and molybdenum, even in quantities as low as 0.003%, promote
the alignment of cementite. Other elements, which also promote banding, are
chromium, niobium, and manganese (Verhoeven et al., 1998, 63). The
effect of the cooling rate on the forging of the ingot and the resulting pattern
has not been studied in any depth. Verhoeven and Jones (1987, 170) note that
cementite at the prior austenite grain boundary form during slow cooling,
whereas faster cooling rates promote Widmanstätten cementite.
Richard Furrer (pers. com.) noted that during his replication experiments
quickly cooled ingots were easier to forge than slowly cooled ingots. This is
probably the result of the different cementite locations. It seems
reasonable to assume that the cooling rate affects the appearance of the
pattern. This is because the faster the ingot cools, the smaller the dendrites
are, and therefore, the closer the interdendritic zones. The closer the
interdendritic zones, the closer the aligned globular/spheroidal cementite are,
and therefore, the finer the final surface pattern. Therefore, a blade forged from a slowly cooled ingot would
have a coarser pattern than a blade forged from a quickly cooled ingot, assuming
that the blades require a similar amount of forging. In addition, Verhoeven and
Jones (1987, 177) suggest that the grain boundary cementite grows coarser with
each forging cycle, opposed to the Widmanstätten cementite, which becomes
finer. It is the large cementite particles responsible for the thicker
“thread” of the Damascus patterns. The extent of forging and consequently
the extent of deformation of the dendrites would also affect the fineness and
appearance of the pattern. The influence of the cooling rate was also noted by
ethnographic accounts. Bronson (1986, 38) states that many ethnographic
observers suggested that the Damascus pattern “is an effect of cooling the
original crucible contents at an extremely slow rate”. Therefore
it seems likely that the fineness or coarseness of the final pattern would
depend on the cooling rate of the liquid steel in addition to the amount of
forging. A slowly cooled ingot could make a coarse pattern or, if forged for a
long period, a fine pattern, but a quickly cooled ingot could never make a
coarse patterned blade but only a fine patterned one. Verhoeven
and Pendray’s (1992, 210) experiments found that the as-cast ingot was “hot
short” due to microsegregation of phosphorus and sulphur. Although few ancient
steels contain sulphur, they often contain phosphorous. Since the ingots
solidified from a liquid, they have areas particularly high in phosphorus
appearing as the iron-carbon, phosphorous phase steadite rather than being
evenly distributed, thus the ingots are “hot short”. Whether ancient blades
were also “hot short” and if this decarburization procedure would have been
needed if the crucibles cooled slowly in the furnace or is necessary for all
crucible steel is uncertain, however, the crucible steel blades examined did
contain areas with around 0.1% P. The findings by Verhoeven, that the
crucible steel ingots were “hot short”, are important for three reasons: 1) It supports the fact that Moxon among others noted that “hot shortness” was a feature of crucible steel. 2) Being “hot short”, the blades required a different forging technique than used for other types of steel. 3)
The low temperature forging would produce spheroidal cementite. The
phosphorous in the ingots caused the ingots to be “hot short” and therefore
they had to be forged at low temperatures. Verhoeven
(2001, 65) found that during forging at the necessary low temperatures, below
the austenite transition temperature, the cementite collects in the
interdendritic regions, perhaps nucleating on the impurity elements, which are
concentrated in the interdendritic regions. The austenite transition temperature
(Acm) is the temperature at which ferrite and cementite begin to
separate during slow cooling (Samuels, 1980, 43). The austenite transition
temperature depends upon the elemental composition of the steel, particularly
the carbon content. The transition temperature begins in the region of 730OC,
around the eutectoid composition (0.8% C). The austenite transition temperature
increases with the carbon content until the carbon content reaches around 2%
(cast iron) where the temperature is over 1100OC (see Samuels, 1980,
43). The
time and temperature of the forging are major factors in the formation of the
pattern. Verhoeven and Pendray’s replication experiments heated the blades to
50OC below the austenite transition temperature and then forged the
blade while it slowly air-cooled to around 250OC below the austenite
transition temperature (Verhoeven, 2001, 64-65). They record that initially the
carbides are randomly distributed but after additional heating and forging at
these temperatures the cementite began to align. The more cycles they performed,
the more distinct the banding became. In
order for the pattern to be readily observed on the surface of the blade, the
decarburized and oxidized layer had to be ground off, the blade had to be
cleaned and polished before it was etched. Wilkinson records that wood-ashes and
water were used in India, or chalk and water to remove any surface grease (1837,
191). Other materials used to clean
the steel include dry lime with water and tobacco ash (Sachse, 1994, 83). To
etch the blades, Wilkinson (1837,191) discusses the use of dilute nitric and
sulphuric acids at Cutch. He also records that a better effect is produced when
the blade is immersed in a bath of copper sulphate in water for ten to thirty
minutes (Wilkinson, 1937, 190-191). Sachse (1994, 84) refers to the use of
ferric sulphate and ferrous sulphate to etch the blades. The etching reacts
preferentially to the iron and carbide regions and the effect depends on the
type of etchant used and the amount of time it reacts with the metal. According
to Verhoeven and Jones (1987, 155) the white component
(a.k.a. threads, see Classification of Damascus Patterns) of hypereutectoid
Damascus patterned blades is the cementite. On hypoeutectoid blades the ferrite
is the white or lighter component. The darker “background” colour is often a form of pearlite which appears darker, or having a
pearl–like appearance, hence the name. However, which phases appear lighter or
darker also depends on the microstructure and the etchant used. In
summary, the formation of the pattern particularly in hypereutectoid blades is
due to the interdependent relationship between the elements contained in the
crucible steel ingot and the forging process. The presence of phosphorous in the
crucible steel dictated the low forging temperature. In turn, the low
temperature forging produced spheroidal cementite. The presence in the ingot of
the trace elements such as vanadium,
molybdenum, chromium, niobium, or manganese promote the alignment of the
spheroidal cementite in the steel, thus producing the Damascus pattern when
etched. The relationship between the elemental composition of the ingot and
forging method associated with hypoeutectoid blades has not been studied
in detail. However, the presence of elements such as manganese promotes the
growth of pearlite in the interdendritic region, whereas the dendrite is
composed of ferrite. Slow cooling of the ingot will produce bigger bands and
these bands can be observed when the blade is etched. |
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