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Materials Characterization 50 (2003) 305–315
Microstructural characterization of controlled forged HSLA-80
steel by transmission electron microscopy
Samar Dasa, A. Ghoshb, S. Chatterjeeb,*, P. Ramachandra Raoa,1
aNational Metallurgical Laboratory, Jamshedpur 831007, IndiabDepartment of Metallurgy, Bengal Engineering College, Deemed University, PO Botanic Garden, Howrah West Bengal 711-103, India
Received 15 July 2002; accepted 15 July 2003
Abstract
In this study, transmission electron microscopy (TEM) was used to evaluate the effect of controlled forging followed by
cooling at various rates on microstructure of an HSLA-80 steel. The observations demonstrate that water-quenched steel has
finer multiphase constituents of lath martensite, bainite and twined martensite, whereas air-cooling has resulted in a mixture of
bainitic ferrite, retained austenite or MA constituents along with some Widmanstatten ferrite. When the steel is cooled in sand,
the maximum volume fraction of polygonal ferrite (PF) was produced which, in turn, increased volume fraction of MA
constituents. Precipitation of fine q-Cu, Nb and Ti carbides and carbonitrides was observed and identified using energy
dispersive spectrometric analysis (EDS) and electron diffraction.
D 2003 Elsevier Inc. All rights reserved.
Keywords: Steel; EDS; TEM
1. Introduction alloying elements provide hardenability for transfor-
Development of HSLA-80 and HSLA-100 steels
have successfully replaced HY-80 and HY-100 steels
in naval applications due to their improved strength,
toughness at ambient and sub-ambient temperatures
along with good weldability and corrosion resistance
properties [1–5]. These steels are generally Cu-bear-
ing and alloyed with Ni, Mn, Mo, Cr, along with Nb,
Ti and V microalloying elements. Most of these
1044-5803/$ - see front matter D 2003 Elsevier Inc. All rights reserved.
doi:10.1016/j.matchar.2003.07.001
* Corresponding author. Tel.: +91-33-2668-4561; fax: +91-33-
2668-4564.
E-mail addresses: [email protected] (S. Das),
[email protected] (A. Ghosh), [email protected]
(S. Chatterjee).1 Present address: Benaras Hindu University, Varanasi 221005,
India.
mation of austenite into fine structures in heavy
sections. This structural homogeneity has enabled
these steels to be used in both offshore and onshore
pipeline and other structural applications. While a
significant quantity of these steels is being produced
through controlled rolling operations, forging has
become a competitive technique for producing such
steels. Forging is an isotropic deformation process
accompanied with high strain rate. Moreover, various
post-forging cooling rates can produce a variety of
microstructures, which ultimately result in different
combinations of strength and toughness in these steels.
The isothermal, continuous cooling transformation and
age hardening characteristics of ASTM 710/HSLA-80
steel have been studied by previous workers [6–10].
The microstructural characterization of as-rolled and
S. Das et al. / Materials Characterization 50 (2003) 305–315306
tempered HSLA-100 steels has also been reported
[11,12]. However, the detailed microstructural charac-
terization of HSLA forging steels has not been ex-
plored so far. In this present study, an HSLA-80 steel
has been subjected to a controlled forging operation
and subsequently cooled in three different mediums,
i.e. water, air and sand. The decomposition product of
the austenite as a result of controlled forging and
different post-forging cooling rates has been evaluated
using transmission electron microscopy (TEM). The
distribution of various precipitates was examined and
identified by energy dispersive X-ray spectroscopy
(EDS) and electron diffraction.
2. Experimental
The steel used in this study was supplied by Naval
Research Laboratory,Washington, DC, andUSA under
an INDO-US collaborative programme. The chemical
composition of the steel is shown in Table 1, which is
an HSLA-80 steel. Steel slabs of 50� 50� 300 mm
were reheated at 1200 jC and controlled forged in two
stages. In Stage I, 50% deformation was applied in
temperature range of 1100–1050 jC and in Stage II
another 50% deformation was given in temperature
range of 850–800 jC. Subsequently, the slabs were
cooled in sand, air and water. The operating temper-
atures were measured by embedding a thermocouple
into steel slabs. Optical metallographic samples, pre-
pared by conventional grinding and polishing techni-
ques, were etched with 2% nital solution and observed
in a light microscope. Volume percentage of different
phases were measured from optical micrographs using
image analyser. For the TEM study, thin slices were cut
by a low speed diamond saw and then subjected to
mechanical grinding. Three millimeter diameter discs
were punched and electrolytically thinned in Struer’s
Tenupol twin jet polisher using a mixture of 90% acetic
acid and 10% perchloric acid. The samples were
evaluated in a Philips CM200 TEM operated at 200
kV. Energy dispersive X-ray spectroscopy (EDS) mi-
Table 1
Chemical composition (wt.%)
C Mn S P Cu Ni Si Cr
0.05 1.0 0.001 0.009 1.23 1.77 0.34 0.6
croanalysis was carried out to determine the chemical
composition of various precipitates.
3. Results and discussion
Different cooling rates from same finish forging
temperature have produced a variety of transformed
microstructures in the final product, i.e. polygonal
ferrite, Widmanstatten ferrite, lath martensite, bainite,
interlath retained austenite and/or MA constituents.
The various transformation products of austenite
formed in different temperature ranges can be classi-
fied using TEM. Polygonal ferrite (PF) is a high
temperature decomposition product of austenite and
can be characterized by the presence of distinct grain
boundaries of polygonal or equiaxed shaped grains
containing a relatively low dislocation density. Acic-
ular ferrite is the highly dislocated non-equiaxed
ferrite that forms on continuous cooling in the tem-
perature range which is slightly higher than that for
the transformation to upper bainite. Bainite can be
characterized by the presence of highly dislocated
ferrite laths with precipitation of carbides at the
interlath or intralath region of ferrite. In upper bainite,
precipitation occurs predominantly at interlath loca-
tions, whereas in lower bainite the precipitates form in
the intralath region [13,14]. The term ‘‘granular bain-
ite,’’ particularly in low carbon steels, has been
described by Bramfitt and Speer [15] to include
aggregates of ferrite of any shape (acicular, polygonal
or featureless) together with retained austenite and/or
MA constituents. The martensitic transformation
product is generally differentiated by its transforma-
tion substructures, i.e. twin substructures (plate mar-
tensite) and dislocated substructures (lath martensite).
3.1. Optical microstructure of the steels at different
cooling rates
Optical microstructure of water-quenched sample
(Fig. 1a) shows a mixture of martensite and bainite.
Mo Ti Al Nb Carbon equivalent
1 0.51 0.03 0.025 0.037 0.69
Fig. 1. Optical micrograph of the steel cooled at different rates; (a)
35 jC/s (water-quenched), (b) 1.15 jC/s (air-cooled), (c) 0.68 jC/s(sand-cooled).
S. Das et al. / Materials Characterization 50 (2003) 305–315 307
Martensite of very fine lath size is observed in packet
form and comparatively coarser laths of bainitic ferrite
have also been noted. The optical micrograph of air-
cooled sample in Fig. 1b shows that the microstruc-
ture is predominantly bainitic ferrite. The acicularity
of fine bainitic ferrite laths was also observed. The
distributions of discrete black regions in the bainitic
ferrite matrix were either retained austenite or mar-
tensite/austenite (MA) constituents. The optical mi-
crograph of sand-cooled sample (Fig. 1c) shows that
the microstructure is predominantly ferrite along with
randomly distributed dark islands. Acicularity and
fineness of the ferrite is decreased, and a polygonal
and/or quasi-polygonal shape has evolved. The size of
discrete second phase particles in the ferrite matrix has
increased compared to that in water-quenched or air-
cooled samples.
3.2. TEM study
3.2.1. Microstructure of water-quenched (cooling rate
35 jC/s) steelWater quenching from the finish forging tempera-
ture of 800 jC has produced generally fine lath
structure of the steel. Fig. 2a shows a low magnifica-
tion bright-field TEM image of highly dislocated lath
martensite packets with flat interfaces. Dispersed
twined martensite islands were observed in the lath
(Fig. 2b). The corresponding dark-field TEM image of
Fig. 2c clearly shows the twinned martensite island in
the intralath position and also at the lath boundary. A
selected area diffraction pattern (SADP) is obtained
from one of these twinned martensite regions and is
shown in Fig. 2d. The schematic illustration of dif-
fraction pattern, Fig. 2e, clearly indicates the matrix
and twin spots along with double diffraction spots.
The matrix has [13̄1]M zone axis and twins to be
[1̄31̄]T indicating that twining has occurred along
(211)M/T plane. The fine twins are generally associat-
ed with high carbon plate martensite due to a signif-
icant enrichment of carbon in austenite. Regarding the
formation of interphase twined martensite Dunne et al.
[7] have speculated based on their experimental
observations that carbon-enriched austenite would
transform to a twin-related ferrite since this path
minimises the accommodation of strain energy gen-
erated by the formation of adjacent plate shaped
crystals of ferrite. Based on earlier observations
[7,16], it was found that the carbon concentration in
the twined martensite was greater than 0.4 wt.% C.
Speich [16] observed that the quenched structure of a
medium carbon steel containing 0.45–0.55 wt.% C
Fig. 2. Transmission electron micrographs of water-quenched steel. (a) Bright-field image shows packet of lath martensite. (b) Higher
magnification bright-field image showing twinned martensite islands. (c) Dark-field image of (b). (d) SADP obtained from one of these twined
martensite regions. (e) Schematic presentation of (d).
S. Das et al. / Materials Characterization 50 (2003) 305–315308
Fig. 3. Transmission electron micrographs of water-quenched steel. (a) Bright-field image shows sheaves of bainitic laths. (b) Bright-field image
showing upper bainite laths containing precipitation of cementite at the lath boundary (arrowed). (c) SADP from interlath region. (d) Schematic
presentation of (c). (e) An enlarged bright-field image of bainitic lath shows intralath needle-shape precipitation of carbide particles. (f) Dark-
field of (e).
S. Das et al. / Materials Characterization 50 (2003) 305–315 309
Fig. 4. Bright-field TEM image of the air-cooled steel. (a)
Formation of Widmanstatten Ferrite (WF) saw teeth; (b) a closer
view of interface of WF where tiny precipitates appear to be
interacting with dislocations.
S. Das et al. / Materials Characterization 50 (2003) 305–315310
should be typically lath martensite with about 20%
twined martensite, though Wenpu et al. [11] have
observed 50% lath martensite and 1% granular twined
martensite in a quenched HSLA-100 steel. In this
controlled forged HSLA 80 steel, the volume percent
of lath martensite obtained is f 55 which is very
close to the observation reported by Wenpu et al. [11].
Approximately 40 vol.% bainite was observed in
the water-quenched steel. Fig. 3a shows a low mag-
nification bright-field TEM image of highly dislocated
upper bainite laths. These laths were up to f 2 Am in
width, which was coarser than the lath martensite size.
The bright-field TEM image in Fig 3b shows precip-
itation of a thin carbide particle at the lath boundaries
(arrowed). The SADP taken from this region is shown
in Fig 3c. The schematic illustration (Fig 3d) indicates
the carbide as cementite and the orientation relation-
ship between orthorhombic cementite and ferrite was
obtained as:
½011̄�aN½2̄01�c and ð011ÞaNð112Þc:
In the higher magnification bright-field TEM im-
age of bainite (Fig. 3e), needle-shaped precipitates
approximately 40–60 nm long and 4–8 nm thick are
observed in the intralath position. A dark band, which
may be an inclined lath boundary, is also visible. In
the dark-field TEM image of Fig. 3f, this dark band is
clearly revealed and it consists of numerous fine
carbide and carbonitride precipitates. Intralath nee-
dle-shaped precipitates are also clearly visible in the
dark-field image.
3.2.2. Microstructure of air-cooled (cooling rate 1.15
jC/s) sampleA change in microstructure was observed when the
steel was cooled in air from the same finish forging
temperature. The bright-field TEM image in Fig. 4a
shows the presence of Widmanstatten ferrite (WF) saw
teeth with a triangular-shaped grain. A reduced dislo-
cation content and low angle grain boundaries are
associated with the WF grains. A view of the interface
in Fig. 4b shows the presence of dislocation tangles
interacting with fine precipitates. Aaronson [17] has
described these type of perturbations at g/a interphase
region as the initial stage of development of Widman-
statten saw teeth. From their experimental evidence,
Thompson et al. [8,9] proposed that Widmanstatten
ferrite growth may be accompanied with precipitation
of Cu particles at the interface between the WF grain
and austenite. The mechanism of formation of WF is
still a matter of debate, but it is in general agreement
that formation of WF occurs at faster cooling rates and
at a lower temperature range than that for polygonal
ferrite. Thus, at the initial stage of air-cooling, austenite
has decomposed into WF and the growth has been
S. Das et al. / Materials Characterization 50 (2003) 305–315 311
accompanied by interstitial as well as substitutional
atom diffusion. However, the structure of air-cooled
steel contains maximum volume fraction of bainitic
ferrite, which has formed at the later stage of air-
cooling. Fig. 5a shows a bright-field TEM micrograph
of bainitic ferrite comprised of acicular ferrite laths
along with an interlath thin film of retained austenite.
The dislocation density was higher than in WF formed
at the initial stage of cooling. The width of the bainitic
ferrite laths varies from f 0.4 to 1.5 Am, and the length
is in the range of f 4.4–5.4 Am. Some blocky darkly
imaging regions were identified as MA constituents. A
bright-field TEM image (Fig. 5b) shows one such
interlath darkly imaging region where fine microtwins
Fig. 5. Transmission electron images of the air-cooled steel. (a) Bright-
austenite and/or MA constituents. (b) Bright-field image shows fine twins
granular ferrite (GF).
are observed. In the dark-field TEM image (Fig. 5c),
the twins are clearly revealed.
The occurrence of granular ferrite during the con-
tinuous cooling transformation of austenite in ASTM
710 steel has been discussed by Thomson et al. [8], and
in the present study similar features have been observed
and are shown in the bright-field micrograph of Fig. 5d.
3.2.3. Microstructure of sand-cooled (cooling rate
0.68 jC/s) sampleThe bright-field TEM micrograph (Fig. 6a) of
sand-cooled steel shows polygonal ferrite with a
reduced dislocation density. The bright-field TEM
image of Fig. 6b shows the polygonal ferrite with
field image shows bainitic ferrite laths with intermediate retained
at interlath dark region. (c) Dark-field of (b). (d) Highly dislocated
Fig. 6. Bright-field TEM image of sand-cooled steel. (a) Polygonal
ferrite (PF), with a low dislocation density. (b) An enlarged view
showing polygonal ferrite with MA constituents.
S. Das et al. / Materials Characterization 50 (2003) 305–315312
dark chunky-shaped MA constituents. The volume
fraction of the second phase (i.e. retained austenite
and or MA constituents) has increased in the sand-
cooled samples.
Very slow cooling from the finish forging temper-
ature of 800 jC in sand has allowed sufficient time for
carbon diffusion in the high temperature range to
obtain the maximum volume fraction of polygonal
ferrite. A large volume fraction of ferrite is associated
with a substantial amount of carbon enrichment in the
austenite. From the CCT diagram of HSLA 80 steel
obtained by earlier workers [7–9], it has been ob-
served that after the completion of ferrite formation,
no further transformation occurs until the bainite start
temperature is reached. The occurrence of the classical
upper bainitic structure was observed for the faster
cooling rate (Fig. 3) where precipitation of cementite
occurred at the ferrite lath boundaries. But at the
slower cooling rates such as those for air- or sand-
cooling, dark chunky-shaped retained austenite and/or
MA constituents were randomly distributed in ferrite
matrix (Figs. 5 and 6b). The maximum extent up to
which the bainitic reaction can proceed depends on
the composition of residual austenite [18,19]. If the
free energy of austenite and ferrite of same composi-
tion are equal, then the bainitic reaction ceases. These
factors lead to the conclusion that after the completion
of polygonal ferrite formation when the equilibrium
carbon concentration between austenite and ferrite has
been reached, austenite has become stable. With
further decrease in temperature, the carbon-enriched
austenite either transforms into twin-related martens-
ite/MA constituents or remained as retained austenite.
3.2.4. Precipitation
One of the prime objectives of this TEM study was
to observe the precipitation behavior of fine micro-
alloying carbides/carbonitrides and q-Cu particles as a
result of the high strain induced in the material during
controlled forging and different post-forging cooling
rates. Faster quenching from finish forging temperature
of 800 jC has suppressed the precipitation except for
some fine carbides and carbonitrides that have been
observed to precipitate at the dislocation networks in
the bainitic lath as described earlier (Fig. 3). Compar-
atively slower cooling in air from the same finish
forging temperature has resulted in a larger distribution
of precipitates (less than 30 nm in size), preferentially at
the dislocation substructure as shown in Fig. 7a. In the
sand-cooled steel, the dark-field TEM image, Fig. 7b,
shows a distribution of fine precipitates (f 8–35 nm in
size) with some coarser precipitates (55–65 nm in size)
in ferrite matrix. The EDS spectrum taken from the
cuboid shape particle (arrowed) in Fig. 7b is shown in
Fig. 7c. The EDS spectrum shows the presence of
several elements, i.e. Ti, Nb and Cu in the particle
Fig. 7. (a) Bright-field TEM image showing precipitation of fine carbides and carbonitrides in the air-cooled steel; (b) dark-field TEM image
showing precipitation in the sand-cooled steel. (c) EDS spectra from the cuboid precipitate (arrowed in b). (d) Corresponding SADP from the
above region. (e) Schematic presentation of (c); (f) bright-field TEM image showing the presence of q-Cu precipitate. (g) Corresponding EDS
spectra from the q-Cu precipitate marked in (f).
S. Das et al. / Materials Characterization 50 (2003) 305–315 313
S. Das et al. / Materials Characterization 50 (2003) 305–315314
which indicates that the particle is complex in nature
and a substantial amount of diffusion of interstitial as
well as substitutional atoms has occurred during slow-
cooling from finish forging temperature of 800 jC. AnSADP from this region shows ferrite reflections along
with precipitate reflections, Fig. 7d. The calculated
lattice parameter of this face-centered cubic precipitate
was 0.4481 nm, which correspond to an Nb(CN)
precipitate. From the schematic illustration of the
SADP (Fig. 7e), the orientation relation between ferrite
and Nb(CN) was obtained as
½3̄11�aII½01̄1̄�NbðCNÞ and ð011̄ÞaIIð200ÞNbðCNÞ
The bright-field TEM micrograph of Fig. 7f shows the
presence of a q-Cu particle (arrowed) in the ferrite
matrix in the sand-cooled steel. The EDS spectrum
obtained from this particle (Fig. 7g) confirms it as q-Cu.The precipitation behavior in a steel of similar
composition was studied by Mishra et al. [20]. They
observed precipitates nearly 100 nm in size located at
the lath boundaries after solutionizing and quenching
from 1100 jC. They had assumed these particles to be
the Nb-rich precipitate, but detailed TEM observations
had not been reported. In this present study, controlled
forging followed by cooling at different rates has
resulted in a more uniform distribution of finer precip-
itates: microalloy carbides, carbonitrides and q-Cu.
4. Conclusions
Controlled forging followed by cooling at different
rates in this HSLA-80 steel has produced the follow-
ing microstructural changes:
(1) Water-quenching from the 800 jC finish forging
temperature has resulted in low temperature
decomposition product of austenite, i.e. f 55
vol.% lath martensite, f 35–40 vol.% bainite
and some twined martensite, retained austenite
and/or MA constituents.
(2) Steel cooled in air was characterized by a
predominantly bainitic ferrite microstructure
along with fine precipitates of microalloying
carbides, carbonitrides, interlath retained austenite
and MA constituents. The lath size was coarser
than that of water-cooled steel. The high temper-
ature decomposition product of austenite, i.e.
Widmanstatten ferrite, was also observed in the
air-cooled steel.
(3) Sand-cooling has resulted in a maximum volume
fraction of polygonal ferrite associated with
precipitation of q-Cu, Ti and Nb carbides and
carbonitride precipitates. Some localized coarsen-
ing of precipitates has been observed. The size
and the volume fraction of second phase, i.e. MA
constituents and retained austenite, have increased
in sand-cooled steel.
Acknowledgements
The authors gratefully acknowledge the financial
support rendered by the Naval Research Laboratory,
Washington, DC, USA under INDO-US programme
for carrying out this investigation.
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