Everything about the steel around us


A brief overview over steel

Steel is a metal alloy whose majorsimilar but less beautiful bainite.
component is iron, with carbon contentPerhaps the most important allotrope is
between 0.02% and 1.7% by weight. Carbonmartensite, a chemically metastable
is the most cost effective alloyingsubstance with about four to five times
material for iron, but many otherthe strength of ferrite. A minimum of
alloying elements are also used.[1]0.4 wt% of carbon is needed in order to
Carbon and other elements act as aform martensite. When the austenite is
hardening agent, preventing dislocationsquenched to form martensite, the carbon
in the iron atom crystal lattice fromis "frozen" in place when the cell
sliding past one another. Varying thestructure changes from FCC to BCC. The
amount of alloying elements and theircarbon atoms are much too large to fit
distribution in the steel controlsin the interstitial vaccancies and thus
qualities such as the hardness,distort the cell structure into a Body
elasticity, ductility, and tensileCentered Tetragonal (BCT) structure.
strength of the resulting steel. SteelMartensite and austenite have an
with increased carbon content can beidentical chemical composition. As such,
made harder and stronger than iron, butit requires extremely little thermal
is also more brittle. The maximumactivation energy to form.
solubility of carbon in iron is 1.7% byThe heat treatment process for most
weight, occurring at 1130° Celsius;steels involves heating the alloy until
higher concentrations of carbon or loweraustenite forms, then quenching the hot
temperatures will produce cementitemetal in water or oil, cooling it so
which will reduce the material'srapidly that the transformation to
strength. Alloys with higher carbonferrite or pearlite does not have time
content than this are known as cast ironto take place. The transformation into
because of their lower melting point.[1]martensite, by contrast, occurs almost
Steel is also to be distinguished fromimmediately, due to a lower activation
wrought iron with little or no carbon,energy.
usually less than 0.035%. It is commonMartensite has a lower density than
today to talk about 'the iron and steelaustenite, so that the transformation
industry' as if it were a single thing;between them results in a change of
it is today, but historically they werevolume. In this case, expansion occurs.
separate products.Internal stresses from this expansion
Currently there are several classes ofgenerally take the form of compression
steels in which carbon is replaced withon the crystals of martensite and
other alloying materials, and carbon, iftension on the remaining ferrite, with a
present, is undesired. A more recentfair amount of shear on both
definition is that steels are iron-basedconstituents. If quenching is done
alloys that can be plastically formedimproperly, these internal stresses can
(pounded, rolled, etc.).cause a part to shatter as it cools; at
Iron, like most metals, is not found inthe very least, they cause internal work
the Earth's crust in an elemental state.hardening and other microscopic
Iron can be found in the crust only inimperfections. It is common for quench
combination with oxygen or sulfur.cracks to form when water quenched,
Typically Fe2O3—the form of iron oxidealthough they may not always be visible.
(rust) found as the mineral hematite,At this point, if the carbon content is
and FeS2—Pyrite (fool's gold). Ironhigh enough to produce a significant
oxide is a soft sandstone-like materialconcentration of martensite, the result
with limited uses on its own. Iron isis an extremely hard but very brittle
extracted from ore by removing thematerial. Often, steel undergoes further
oxygen by combining it with a preferredheat treatment at a lower temperature to
chemical partner such as carbon. Thisdestroy some of the martensite (by
process, known as smelting, was firstallowing enough time for cementite,
applied to metals with lower meltingetc., to form) and help settle the
points. Copper melts at just over 1000internal stresses and defects. This
°C, while tin melts around 250 °C.softens the steel, producing a more
Steel melts at around 1370 °C. Bothductile and fracture-resistant metal.
temperatures could be reached withBecause time is so critical to the end
ancient methods that have been used forresult, this process is known as
at least 6000 years (since the Bronzetempering, which forms tempered steel.
Age). Since the oxidation rate itselfOther materials are often added to the
increases rapidly beyond 800 °C, it isiron-carbon mixture to tailor the
important that smelting take place in aresulting properties. Nickel and
low-oxygen environment. Unlike coppermanganese in steel add to its tensile
and tin, liquid iron dissolves carbonstrength and make austenite more
quite readily, so that smelting resultschemically stable, chromium increases
in an alloy containing too much carbonthe hardness and melting temperature,
to be called steel.and vanadium also increases the hardness
Even in the narrow range ofwhile reducing the effects of metal
concentrations that make up steel,fatigue. Large amounts of chromium and
mixtures of carbon and iron can formnickel (often 18% and 8%, respectively)
into a number of different structures,are added to stainless steel so that a
or allotropes, with very differenthard oxide forms on the metal surface to
properties; understanding these isinhibit corrosion. Tungsten interferes
essential to making quality steel. Atwith the formation of cementite,
room temperature, the most stable formallowing martensite to form with slower
of iron is the body-centered cubic (BCC)quench rates, resulting in high speed
structure ferrite or ?-iron, a fairlysteel. On the other hand sulfur,
soft metallic material that can dissolvenitrogen, and phosphorus make steel more
only a small concentration of carbon (nobrittle, so these commonly found
more than 0.021 wt% at 910 °C). Aboveelements must be removed from the ore
910 °C ferrite undergoes a phaseduring processing.
transition from body-centered cubic to aWhen iron is smelted from its ore by
face-centered cubic (FCC) structure,commercial processes, it contains more
called austenite or ?-iron, which iscarbon than is desirable. To become
similarly soft and metallic but cansteel, it must be melted and reprocessed
dissolve considerably more carbon (asto remove the correct amount of carbon,
much as 2.03 wt% carbon at 1154 °C)[2].at which point other elements can be
As carbon-rich austenite cools, theadded. Once this liquid is cast into
mixture attempts to revert to theingots, it usually must be "worked" at
ferrite phase, resulting in an excess ofhigh temperature to remove any cracks or
carbon. One way for carbon to leave thepoorly mixed regions from the
austenite is for cementite tosolidification process, and to produce
precipitate out of the mix, leavingshapes such as plate, sheet, wire, etc.
behind iron that is pure enough to takeIt is then heat-treated to produce a
the form of ferrite, and resulting in adesirable crystal structure, and often
cementite-ferrite mixture. Cementite is"cold worked" to produce the final
a stoichiometric phase with the chemicalshape. In modern steelmaking these
formula of Fe3C. Cementite forms inprocesses are often combined, with ore
regions of higher carbon content whilegoing in one end of the assembly line
other areas revert to ferrite around it.and finished steel coming out the other.
Self-reinforcing patterns often emergeThese can be streamlined by a deft
during this process, leading to acontrol of the interaction between work
patterned layering known as pearlite duehardening and tempering.
to its pearl-like appearance, or the



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