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Here is the list of names around steel from the
backbone: |
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- Cementite (German: Zementit). The stoichometric Fe3C
phase. It is a compound with a complicated lattice and rather hard and brittle.
- Ferrite (German: "Ferrit). The a-phase
with the bcc lattice. If you want to be precise, you call it a - ferrite.
- Austenite (German "Austenit). The g-phase with the fcc lattice.
- Pearlite (German: Perlit), the two phase mixture obtained right below
the eutectoid point at 0.8 % C
concentration
- Ledeburite (German: Ledeburit); the two phase mixture obtained right
below the eutectic point at 4.5 % C
concentration.
- Martensite (German: Martensit); a kind of metastable version of
austenite + carbon; but with a tetragonal
lattice and different mechanical properties.
- Bainite (German: Bainit); a mixture of a
- ferrite supersaturated with carbon and cementite, but in a (non-equilibrium) structure
quite different from pearlite.
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How did those names come into beeing? Let's
see: |
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The name Cementite - you might have guessed it - has
something to do with the english word "cement", meaning something that binds or glues
things together in this context. |
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In the words of a dictionary. "In
1885, Osmond and Werth published their "Cell-Theory", in which
not only the existence of allotropic forms of iron was proposed (now known as
austenite and ferrite), but in which also a new look at carbide formation was
given. Their research on high-carbon steels, showed that the matrix consisted
of grains or cells of iron, encapsulated by a thin layer of iron carbide.
During solidification, iron globules, or cells, are formed first and continue
to grow. The remaining melt solidifies as ironcarbide. In this way, the
carbide-phase actually glues or binds the previous formed cells together. This view
makes it understandable why Osmond called the iron-carbide thus formed,
"Ciment" (French for binder or
cement)". |
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Since English and German have words quite similar
to the french ciment, the precise name did
not stick globally but is "cementite"
in Englisch and "Zementit" in
German. |
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Ferrite is
practically self-explaining: |
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Ferrum is the
Latin root for many modern words around iron and iron compounds. The word
ferrum is possibly of Semitic origin. |
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Austenite was
named after Sir William Chandler Roberts-Austen, a British metallurgist
(18431902). |
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Roberts-Austen published the first iron-carbon phase diagram;
in preliminary form 1897 (below), and in a "final" form in
1899. |
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He is also remembered for being the first scientist who
perfomed a quantitative measurement of diffusion in the solid state (Au
in Pb) after A. Fick
established his diffusion laws. |
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Pearlite has
its name frorm the pearl-like luster and iridescence of its appearance. |
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I could not yet find out, who coined this name
and made it stick. |
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However, quite recent research can provide an
explanation why this particular structure is pearl-like in appearance: The
regular spaced lamellae of optically quite different materials form a kind of
"photonic
crystal" with optical properties quite different from those of the
constituents. Real pearls get their luster from the same mechanism; the name
"Pearlite" thus is more fitting than its inventor could have
known. |
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Ledeburite is
named after Adolf Ledebur (1837-1916). |
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Ledebur was
the first Professor for "Eisenhüttenkunde" at the (famous)
Bergakademie Freiberg. In 1882 he discovered the iron-carbon
"Mischkristalle" and became relatively famous. "Ledeburite"
as a name for the iron - cementite eutectic was adopted in honor of his
achievements. |
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Martensite was
named after Adolf Martens (1850 - 1914). |
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Martens started as an engineer, made it to the
director of the royal mechanical laboratory, which evolved into the
"Staatliche Materialprüfungsamt" in Berlin. In Germany, a
prestigious prize is now awarded in his name. |
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Bainite is
named after the American chemist E. C. Bain. In the words of an US
source: |
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"The history of austempering begins in the
1930's, when Grossman and Bain, working for the United States Steel
Laboratories, were evaluating the metallurgical response of steels cooled
rapidly from 1450°F (788C) to intermittently high temperatures and
held for various times. The outcome of their pioneering research is what we now
commonly call the "isothermal transformation diagram" Grossman and
Bain were familiar with the conventional metallurgical structures of ferrite,
pearlite and martensite. What they discovered, however, was another structure,
formed above the martensite start temperature (Ms) and below the pearlite
formation region. In steels, this structure took the form of an acicular
(plate-like) structure with a feathery appearance. X-ray diffraction later
identified this structure as a combination of ferrite and metal carbide. The
resultant structure, termed "Bainite" was found to be stronger and tougher
than a comparable "quenched and tempered" structure. |
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© H. Föll (MaWi 1 Skript)