A STUDY OF PRECIPITATION D. J. DYSON?
IN A 1233--Co-M0
STEEL*
and S. R. KEOWNT
The structural changes occurring during the tempering of a 12 %Cr-6%Mo-10 %Co-0.1 %C steel have been investigated. It has been shown that an intermetallic compound R-phase is responsible for the marked secondary hardening but that the carbides M,X and M& are also precipitated. The R-phase contained iron, chromium and molybdenum but little or no cobalt. By determining the orientation relationship between R-phase and ferrite it has been shown that the precipitation of R-phase in ferrite is theoretically favourable. ETUDE
DE
LA
PRECIPITATION
DANS
UN
ACIER
1233-43~-MO
Les variations de structure se prod&ant au tours du revenu d’un acier 12 %Cr-6 %Mo-10 %Co-0,I %C ont et& Qtudiees. Les auteurs montrent qu’une phase oonstituee par un compose interm&allique R est responsable du durcissement seoondaire prononce, mais qua les carbures M,X et M& prcicipitent bgalement. La phase R contient du fer, du chrome et du molybdene mais peu ou pas de cobalt. En determinant la relation d’orientation entre la phase R et la ferrite, les auteurs montrent que la precipitation de la phase R dans la ferrite est favori& par la theorie. EINE
UNTERSUCHUNG
DER
AUSSCHEIDUNG
IN
EINEM
12 %Cr-Co-Mo-Stahl
Die w&rend des Temperns von 12 %Cr-6 %Mo-10 %Co-0,l %C-Stahl auftretenden Strukturanderungen wurden untersucht. Es wurde gezeight, da13eine R-Phase einer zwisohenmetallischen Verbindung fur die ausgepragte sekundare Verfestigung verantwortlioh ist; jedoch scheiden sich auoh M,X- und M,C-Karbide aus. Die R-Phase enth< Eisen, Chrom und Molybdlin, jedoch wenig oder gar kein Kobalt. Durch Bestimmung der Orientierungsbeziehun~ zwisehen R-Phase und Ferrit wird gezeigt, dal3 die Ausscheidung der R-Phase in Ferrit theoretisoh giinstig ist.
1. INTRODUCTION
Only recently have steels been developed whose properties depend upon the precipitation of intermetallic compounds. Early work on the aging reactions in lZ%Cr steels with large MO and Co additions attributed the high strengths achieved on tempering to the precipitation of Laves and chi phases(ig). In addition an ordered phase, thought to be Fe&o, has been reported. (3) In all this work the precipitates were identified from polycrystalline electron diffraction patterns or, when possible, from X-ray diffraction patterns. With recent advances in the identification of phases by selected area electron diffraction in the electron microscope(4) it has become possible to identify individual precipitate particles from single crystal electron diffraction patterns. The purpose of this work, therefore, was to investigate more fully the nature of the precipitating phases responsible for the strengthening of a stainless 12 %Cr--CO-MO steel. The secondary hardening characteristics of five steels with varying cobalt and molybdenum additions to a basic 12 %Cr-O.l %C composition have previously been reported,(5*6) and the hardness curves are reproduced in Fig. 1. It is clear that the S%Mo100/,0 and 9 %iVZo-15 %Co steels age-harden appreciably more than the steels containing smaller
amounts of molybdenum and cobalt. Increasing the molybdenum content of these steels above 4% appeared to give the maximum hardening and the cobalt was added in the amounts required to balance the ferrite-forming tendencies of the molybdenum. While the two steels with the highest cobalt and molybdenum additions gave similar age-hardening effects, the 9%M?3-15 %CO steel contained an appreciable amount of undissolved chi phase. The steel with the smallest alloy additions i.e. the 6% No-10 %Co steel, was therefore chosen for the present investigation. 2. EXPERIMENTAL
PROCEDURE
The steel was manufactured as a 25 lb. air-melted commercial purity cast of the following composition (wt. %) : -
C
Mn
Si
Cr
MO
co
0.11
0.51
0.26
11.50
6.05
9.60
The ingot was forged to +j in. diameter bar which was then hot rolled to 0.075 in. strip. Specimens were solution treated at 1050°C for 1 hr and water quenched before tempering for 1 hr at temperatures between 450’ and 700°C. Extraction replicas were prepared by etching * Received November 19, 1968. polished specimens in 5 % HCl in Picral and stripping t Swinden Laboratories, Midland Group, British Steel in 5 *A HCl and 10% HNO, in alcohol. Some replicas Corporation,Moorgate, Rotherham, Yorkshire. ACTA METALLURGICA,
VOL.
17, AUGUST
1969
1995
ACTA
1096
METALLURGICA,
VOL.
Ii,
1969
(....
“-y..
/
/.”
FIG. 1. Tempering
‘. \
curves of 12%Cr-CO-MO
steels.
were examined by electron probe microanalysis as electron microscopy. fluorescence
analyses
potentiostatic foil
microscopy
of
suitable
diffraction
residues
techniques”)
specimens
material
X-ray
extracted
were for
also
a thickness
transmission
of
using
made.
were prepared by machining to
as well
and X-ray Thin
electron
the 0.075 in.
0.030 in.
before
heat
treatment, and finally chemical thinningf8) and electropolishing in a chromic-phosphoric 3. MICROSTRUCTURAL
electrolyte.
the
structure
solution
OBSERVATIONS
consisted
stringers
treated of
increase in hardness. 600°C
to
positive Fig.
produce
5(a),
separate identified
Specimens slight
microstructural and
precipitate
martensite
the
with
of delta ferrite and undissolved
micro-
the
first
particles
of
two
at very
quite high
The acicular particles were
carbide
cipitates as the intermetallic condition
gave
for precipitation,
were detected
Fig. 5(b).
as the M,X
aged for 20 min at
overaging evidence
morphologies
magnification,
3.1. Solution treated specimen In
FIG. 2. Optical microstructure of solution treated specimen, showing delta ferrite (f) and chi-phase (c) in heavily segregated regions x 1000.
and the angular pre-
R-phase at later stages of
aging when the particles were larger and more widely
occasional
spaced.
chi phase,
more clearly shown in Fig. 5(c).
The two types of precipitate
morphology
are
It can be seen from
Fig. 2. The shape and size of the ferrite areas enabled
Figs. 6(a) and (b) that there was a very dense distri-
them
bution of precipitate
to be easily
phase.
The
occasional surface
distinguished
ferrite
and
merely
showed
ferrite, chi and martensite dislocation
chi were
those
only
readily
of chi
present
more heavily segregated regions.
replicas
microscopy
from
in
Although
the outline
of the
phases, Fig. 3(a), thin foil
showed
the
vast
difference
in
density between the ferrite, Fig. 3(b), and
part#icles in this slightly overaged
condition. With aging temperatures
up to 700°C the particles
of R-phase slowly increased in size, Figs. 7(a)-(c)
and
then at 750°C the particle size increased quite rapidly. The relationship between the precipitate size of Rphase and hardness is shown in Fig. 8 from which it
the martensite,
Fig. 3(c).
can be seen that there was a linear decrease in hardness
Tempered
specimens
but a further increase in size to about 3000 A did not
3.2.
On tempering,
very
with increasing precipitate little microstructural
was observed until just after maximum hardness. Tempering for short periods
change secondary at 600°C
indicated that the time required for maximum agehardening was very critical. The isothermal aging curve for the steel tempered at 600°C is shown in Fig. 4 and it can be seen that increasing the aging time from 5 to 10 min resulted in about 100 HV
size from 100 A to 1000 A,
cause much further change in hardness. The acicular M,X phase persisted to 65O”C, but at 700°C the needles were replaced by angular particles identified as the M,C carbide. The morphologies of the M,C and the R-phase were clearly very similar at 7OO”C, and M,C could only be positively detected by electron diffraction analysis. As the structure
of the martensite
became
more
DYSOS
AND
KEOWN:
PRECIPITATION
IN
A
lZ”/;Cr-CO-MO
1097
STEEL
FIG. 3(a) FIG. 3(b)
rT “”
; ?
560
,? I
540 520 500
I 10
Time
FIG. 4. Isothermal
4. THE
tempering curve for 12%Cr-6%MolO%Co steel.
be explained
FIG. 3. Microstructure of solution treated specimen. (a) Surface replica showing delta ferrite and chi-phase in martensite. x 4000 x 6. rho Dislocations i” delta ferrite. Thin foil. , . (c) Dislocations in martensite. Thin foil. x 60,000.
unit cell.
in terms of a hexagonal
The parameters (a) hexagonal :
to
the
coarsening
of
apparent that there was a marked decrease in dislocation density compared with the original martensitic The precipitation of R-phase in the delta structure. ferrite was much denser than in the martensite,
see
diffrac-
system can
or rhombehedral
are :
a, = 10.903 A : a, = 9.005 .& x
the
precipitates at 650°C it was possible to detect the remnant dislocations in the structure, Fig. 9. It was
Fig. 6(a).
R-PHASE
ca = 19.342 A (b) rhombohedral
due
OF
et aZ.(s) have shown that the X-ray
tion pattern of R-phase in the Mo-Cr-Co
FIG. 3(c)
resolvable,
thnutes
CRYSTALLOGRAPHY
Komura
clearly
-
50
4u?
30
20
= 74°31.2’
The space group is thought to be R 3-C$. The X-ray powder diffraction patterns of the residue extracted from the specimen heat-treated at 700°C showed broad diffuse lines indicative of a particle size of ~500 8. This was confirmed by the electron microscope observations. The lines were identified as the strong lines of R-phase.
EO
ACTA
1098
METALLURGICA,
VOL.
17,
1969
Fra. 5(b)
Fra. 6(a)
structural
similarities
compounds
between
systems,(g-12)
see
Table
tion for certain R-phase
intermetallic
of the electron
phase
M,Moso3)
explain
offer an explanation Figures diffraction
10 and
diffraction
in terms
patterns
of a second
However,
some patterns,
11 were typical obtained.
whilst
this
R-phase
can
of the electron
Both
show
The patterns as indexed,
illustrate the space group proposed The reflections
careful
for them all.
patterns
Laiie zone orders.
a
Indeed a possible explana-
can be found
can reasonably
intermetallic
in ternary alloy
1, necessitates
analysis of such patterns. from
several
which occur particularly
forming
several serve to
by Komura
Fig. 10 define a [22.1] crystal zone as indexed. curvature
FIG. S(c) FIG. 5. Microstructure of specimens showing M,X and R-phase precipitation. (a) Precipitated particles in tempered martensite. Thin foil. Aged at 600°C for (b) Acicular and spheroidal pre20 min. x 80,000. cipitates in tempered martensite. Thin foil. Aged at (c) Acicular and spheroidal 600°C for 20 min. x 200,000. precipitates in tempered marten&e. Thin foil. Aged at 600°C for 1 hr. x 100,000.
With such large lattice parameters it is expected that electron diffraction patterns from simple index [UV.W] zones will contain several Laiie zone orders since the planes of the reciprocal lattice normal to these directions will be very close together. The close
et al.
the zero order Laiie zone of The
of the median line of this zero order Laiie
zone suggests a tilt of -12”
from [2%1].
reflections
in higher
orientation
is nearer [X.2].
Laiie zones suggest the This is lO”43’ from [22.1].
order
The stronger
The ferrite pattern in Fig. 11 comes from both the [113] and [115] crystal zones which are 9’27 The
orientation
relationship
using the intermediate
has been
[114] zone.
Laiie zone of the precipitate
pattern
apart.
determined
The zero order defines a [12.i]
crystal zone, although its curvature suggests an orientation -12’ from this. The stronger reflections from higher order zones taken together define a [27.6] crystal zone which is 12’43’ from [12.i]. Figure 12 shows the stereographic projection corresponding to this pattern. The orientation relationship common to the solution
DYSOR
AND
KEOWh’:
PRECIPITATION
IN
A
12%Cr-CO-MO
STEEL
FIG. 6. Microstructure of specimen aged at 600°C for 1 hr. (a) Extraction replica showing dense precipitation in martensite and even heavier precipitation in the delta ferrite. x8000. (b) Extraction replica of M,X and R-phase in the marten&e. x 100,000.
of all the electron diffraction p&terns (10.0) R-phase -//
taken was:
(32i) ferrite
(01.0) R-phase -_I/ (213) ferrite (li.0)
R-phase -_I/ (132) ferrite
(00.1) R-phase
FIG. 6(b)
// (111) ferrite
In general, exact parallelism of precipitete and matrix planes is seldom seen in the diffraction patterns. The ferrite planes of simple indexing which almost form a set of hexagonal axes and which are closest to the unit cell faces of R-phase were chosen to define the above relationship. The sign ambiguity associated with the indexing of single crystal patterns(4) gave rise to several different possible relationships. Only the above one was common to all the patterns.
ACTA
1100
METALLURGICA,
VOL.
15,
1969
Fla. 7(b)
FIG. 7(a)
600
I
4ool 0
SW
VXO Meen
FIG,
from
8. The
2,000 Diameter
3,000
2.500
1500
8,
relationship between hardness and precipitate particle size.
a sample
following
1,500 Preclpltaie
treated
composition
at 700°C for 1 hr gave the (at. %) :
Fe
Cr
MO
co
44.8
25.6
27.8
1.8
FIG. 7(C) FIG. 7. Effect of increasing aging temperature on pre-
cipitate particle size. (a) Aged at 600°C for 1 hr. Extraction replica x 16,000. (b) Aged at 650°C for 1 hr. Extraction replica. x 16,000. (c) Aged at 700°C for 1 hr. Extraction replica. x 16,000. 5. ELEMENTAL
Electron together
ANALYSIS
probe microanalysis
with X-ray
fluorescence
OF R-PHASE
of extraction
replicas
analysis of some of
the extracted residues separated for X-ray diffraction analysis has enabled the approximate composition of R-phase to be established. X-ray fluorescence analysis of a residue extracted
Electron probe microanalysis of an extraction replica from a specimen tempered at 700°C for 1 hr confirmed
that the phase was rich in iron, chromium
and molybdenum and contained little, if any, cobalt. These analyses showed that although the steel had a very large cobalt addition, the cobalt content of the precipitating phase was very small. Thus the R-phase in this steel was an Fe-Cr-Mo compound. However since the residue used for fluorescence analysis and the replica used for microanalysis both contained carbides it was not possible to define the exact chemical composition
of the R-phase.
DYSON
KEOWN:
AND
PRECIPITATION
FIG. 9. R-phase precipitates and dislocations in martensite aged at 650°C for 1 hr. Thin foil. x 120,000. 6. DISCUSSION
6.1.
Relationship
OF
RESULTS
between microstructure
and hardness The extensive age hardening and retarded softening in this 12 %Cr-6 %Mo-10 %Co stainless maraging steel can be attributed to the very heavy dispersion of precipitates produced during tempering. Initially there is a solid solution hardening effect produced by the high alloy content, augmented by a strengthening contribution from the high dislocation density and the fine grain size of the martensite. On tempering a two stage hardening reaction occurred, M,X precipitating at 550” to 600°C followed by the intermetallic R-phase at 600°C. Maximum hardness at 600% coincided with the heaviest dispersion of carbide and intermetallic particles. The softening of the alloy with further tempering was associated with the growth of the precipitate particles, Fig. 8. The M,X carbide TABLE 1. Comparison
of lattice parameters
IN
A
12%Cr-CO-MO
STEEL
1101
eventually transformed to M,C but it is not known whether on high temperature tempering the R-phase particles merely grew in size or whether they transformed to a different intermetallic phase such as chi or sigma phase. Certainly at very high temperatures chi is the stable phase since it was detected after solution treatment at 1050°C. The microstructure of the specimen tempered to give maximum hardness was extremely complicated. The dislocations were unresolvable and diffraction patterns failed to show any evidence of precipitates or pre-precipitation zones. There was no streaking of the matrix reflections which eliminated the possibility of disc or rod-shaped zones, but not spherical zones which could have been present. Although diffraction effects were obtained from the precipitates present after tempering at 600°C for 1 hr, the particles were too closely spaced to enable single crystal patterns to be recorded. It was not possible to identify the spherical particles as R-phase until the alloy wa,s tempered at 650°C when single crystal patterns were obtained. A noticeable feature of the thin foil microstructure was the absence of dislocations in the overaged condition. It is possible that the misfit between the precipitate and the matrix is sufficiently large for the dislocations to be accommodated at the growing precipitate-matrix interface. 6.2. The significance of the orientation relationship
It can be seen from Fig. 14 that the precipitation of R-phase in ferrite according to the derived relationship requires relatively small atom movements, and therefore represents a low energy transformation. In this diagram the outline of the base of the hexagonal unit cell of R-phase has been superimposed on the projection onto (111) of the atoms in ferrite. The cell faces have been set parallel to (321) ferrite planes. The repetitive volume in ferrite defined by the projected of some transition
metal intermetallic
phases
Crystal structure Phase system Iron-Chromium (T Iron-Molybdenum o Fe,Mo, (p) Fe,Mo, (1~) Fe,Mo Laves Phase R Phase (Mo-Co-Cr) R Phase (Mo-C+Cr) 6 Phase (Mo-Ni) P Phase (Mo-Ni-Cr) x Phase (Fe-Cr-Ni) 12
Tetragonal Tetragonal Hexagonal Rhombohedral Hexagonal Hexagonal Rhombohedral Tetragonal Orthorhombic Cubic
%A 8.800 9.188 4.746 8.928 4.727 10.903 9.005 9.108 9.070 8.860
%?A 8.800 9.188 4.746 8.928 4.727 10.903 9.005 9.108 16.983 8.860
%A 4.544 4.812 25.78 8.928 7.704 19.342 9.005 8.852 4.752 8.860
c(
30”47’
74”31’
llQ2
ACTA
METALLURGICA,
VOL.
.
ZONE
AXE -
FIG. 10, Electron diffraction pattern from
17,
1969
l
N 12’p
[744 FROM
(25.2
R-phasssnd its interpretation.
DYSON
AXTI
KEOWN:
PRECIPITATION
IN
A
12’+oCr-Co-Mo
STEE
ZERO LAUE
ORDER ZONE
F<
PRECIPITATE
SOL”’
Fra.
TO PATTERN PRECIPITATE
11. Electron
FROM
diffraction pattern from R-phesc
and fcrrite and its interpretation
ACTA
METALLURGICA,
VOL.
17,
1969
..OO.tR
111F
---I
--
I
FIG. 12. Stereographic projection corresponding to Fig. 11.
--...
ATOMS
I@;i Wa. 13. Projection of atoms in a-iron
ABOVE
onto (I 11).
PLANE
AT
OF
A
DYSON
base of R-phase R-phase
KEOWN:
and a height ?
contains
favourably
AND
the c,, parameter
168 metal atoms.
This
of
compares
with the 159 metal atoms in the R-phase
unit cell.
The a,, parameter
indicated
10.725 11 and thus an expansion necessary to fit in the intermetallic perpendicular
to
corner distance contraction R-phase
PRECIPITATION
this
plane,
of only 1.66 % is unit cell. Similarly,
the
cell
corner-cell
is 19.861 b thus requiring
to fit the R-phase cell
in Fig. 13 is
cell.
necessary
shows
that
many
of the movements
Other
atoms
which
approach
distances.
require
larger
the
However
magnitude
evidence of the orientation
the
movements
atom
necessary
for
explains
required to convert the transition
strains
cell of ferrite to the
the preferential
Further evidence
theoretically
are found to be large.(14) This precipitation
of the validity
relation is found in terms of the Patterson
precipitate
For a phase whose atomic
if the metallurgical
con-
ditions are favourable. The
atom
Komura
positions
position in
R-phase
et aZ.(g) have been plotted
according
to
as full circles in
Fig. 14. This diagram is one of a series of four which divide equal
the height sections.
tionship,
of the unit cell of R-phase
Using
the derived
the ferrite atoms
have
orientation
into rela-
been superimposed
on Fig. 14 in their relative positions
and are denoted
by open circles. These atoms define planes. Since these planes have been four groups, each open circle represents different heights. The height of the
the 24 (111) divided into two atoms at “first” {ill}
plane above the basal plane of the R-phase cell was chosen such that the sum of the magnitudes of the vertical movements of all atoms to change from their positions in ferrite to those in R-phase, was a minimum.
of two atoms
of R
of the orientation
R-phase cell are thus very small and the latter should in the former
per
between sigma phase and ferrite is known
rather than sigma phase in ferrite.
lattice
moved
relationship
probably
The
of
inter-atomic
the average distance
consist of 24 equally spaced layers of atoms, i.e. 8 of 13.
of
atom remains small.
the
Fig.
distances.
movements-some
relationships
in
1105
are much less than interatomic
Whilst no experimental
a 2.61%
The height of the
ferrite
This diagram
STEEL
proposed
shown
be 4 [ill]
lB%Cr-Co-MO
A
and will thus
units
will
IN
structure
projection.
is based on the
the Patterson
projection
certain planes shows peaks in the same positions
on as
the atoms projected onto that plane. Such is the case for the (111) projection of a-iron, Fig. 13. The close similarity between such a projection projection further
for
R-phase
confirmatory
an
and the Patterson
(00.1)
evidence
of
Fig.
15cg) offers
the
orientation
relationship. 6.3. The role of cobalt It is interesting to outline the role of cobalt in this 12 %Cr-6 %Mo-10 %Co steel. The cobalt is added as a control element to offset the ferrite-forming tendency of molybdenum. Cobalt is an efficient austenite forming element with the added advantage of not depressing
the M, temperature.
It has been shown
ACTA
1106
METALLURGICA,
VOL.
17,
1969
FIG. 15. Patterson projection of R-phase on (00.1) (after Komura et cd.(“)).
that with cobalt
additions
of up to 15 % there is a
hardness
increment
of approximately
wt. %Co
in
steels,(Q
maintained extensive 75 %Co) y-Fe
12 %Cr
at all tempering solid
solubility
and complete
so that
this
9 HV
increment
temperatures.
of cobalt
all the cobalt
1
being
There is
in a-Fe
solid solubility
per
(up to
of cobalt
in
in the 12 %Cr-6%Mo-
10 %Co steel is easily accommodated
in solid solution.
and perhaps this contributes solid solution hardening, Bannerjee
et ai. (15*16)have shown that cobalt increases
the precipitate steels
in some way, other than
to the strength of the steel.
and
nucleation
have
suggested
stacking fault energy number of dislocations tion by discouraging
that
cobalt
maraging lowers
the
of the matrix, increasing the available as sites for precipitacross slip.
suggested
possible
hardening
molybdenum(17~18) or that cobalt orders the matrix.(19)
can
The present work has merely shown that cobalt remains in the matrix and does not enter into the
application if
cobalt
as
a precipitation
intermetallic
compounds
be
produced in steels. From the results of the present work it appears that little or no cobalt is entering into the precipitating cobalt
which
hardening
R-phase
initially
and therefore
imparts
in the solution
useful
treated
the 10% solid
condition,
of
solution main-
tains the solid solution hardening effect throughout the tempering reactions. It is interesting to note that on tempering at 600°C or at higher temperatures, when there is a large volume fraction of precipitate particles and a corresponding decrease in the matrix volume, the matrix will contain considerably
more than 10 % of
cobalt so that cobalt will contribute extra solid solution hardness. However the iron, chromium and molybdenum concentrations in the matrix are being reduced because
as the amount of R-phase increases and molybdenum is a much more potent solid
cobalt
Other workers have
Cobalt does not form carbides in steels but it has a agent
that
rate in 18%Ni
decreases
the
solubility
of
It is suggested however that precipitating phase. cobalt has two distinct effects on the matrix. Firstly the cobalt
affects
the precipitation
of intermetallic
phases by stabilising the nucleating dislocations, not necessarily by lowering the stacking fault energy, at temperatures where normally they would begin to anneal out. Secondly there may be a strengthening effect such as matrix ordering due to the matrix containing cobalt concentrations cobalt content of the steel. 7. SUMMARY
AND
in excess
of the
CONCLUSIONS
An investigation changes occurring
has been made into the structural in a 12 ‘ACr-6 %Mo-10 %Co stainless maraging steel. From the results of this work the
solution hardener than cobalt the total solid solution hardening is not likely to increase. It is not known
following conclusions have been reached : (a) The extensive age hardening and retarded softening was mainly due to the precipitation of the
however what properties a high cobalt matrix possesses
intermetallic
compound
R-phase.
DYSON
AND
KEOWN:
PRECIPITATION
(b) The normal carbide reaction produced in 12 %Cr steels, namely I$X + M,C is superimposed on the intermetallic compound precipitation reaction. (c) It was shown that the R-phase contained iron, chromium and molybdenum but little or no cobalt. (d) The orientation relationship between R-phase and ferrite was determined to be : (10.0) R-phase N /I (3x) (01.0) R-phase -
ferrite
// (213) ferrite
(1i.O) R-phase N // (152) ferrite (00.1) R-phase
// (111) ferrite
(e) From the above relationship it has been shown that only minimal atom movements and small lattice strains are required for R-phase to precipitate from ferrite. Thus R-phase precipitation appears more favourable than the precipitation of sigma phase from ferrite containing suitable alloying elements. ACKNOWLEDGMENTS
The authors wouId like to thank Mr. F. B. Pickering for numerous discussions and continued encouragement and also Dr. F. I-I. Saniter, O.B.E., Director of Research for permission to publish this work.
IN
A
12~oCr-Co-Mo
STEEL
1107
REFERENCES 1. FL J. IRVINE, J. Iron Steel In&. 200, 820 (1962). 2. A. KASAK, V. K. CHANDHOKand E. J. DULIS, Trans. Am. Sot. Metals56, 455 (1963). 3. E. DIDERRICH,D. COUTSOURADIS and L. HABRAKEN,MBm. scient. Revue. M&all. 61. 655 (1964). 4. K. W. ANDREWS, D. J. *Dvsok and S. R. KEOWN, Interpretation of E&xtron Diffraction Patterns. Hilger & Watts (1967). 5. K. J. IRVINE and F. B. PICKERING,Ivwn and Steel Iv&. Special Report No. 86 (1964). 6. K. J. IRVINE, Proc. Brzcssels Int, Conf. on Applications of Cobalt i 1964 1. H. HU&Es,‘J. Iron Steel Inst. 204, 804 (1966). i: S. R. KEOWN and F. B. PICKERING,J. IronSteel In&. 200, 757 (1962). W. G. SLY and D. P. SHOEMAKER, Acta 9. Y. KOMURA, crystallogr. 13, 575 (1960). 10. D. P. SHOEMAKER,C. B. SHOEMAKER,and F. C. WILSON, Acta cry8taZZogr. 10, 1 (1957). and D. P. SHOEMAKER,Acta crysta2Zogr. 11. C. B. SHOEMAKER 10, 997 (1963). 12. C. B. SHOEMAKER,D. P. SHOEMAKERand J. MELLOR, Acta c~~~l~og~. 18,37 (1965). Third Eur. Conf. os Electron 13. S. R. KEOWN, Proe. Microscopy. Prague ( 1964). 14. D. J. DYSON, Unpublished work. 15. R. R. BANNERJEEand J. J. HAUSER, Tv-ansfoymation and Hardenability in steel, p. 133, Climax Molybdenum Co. (1967). 16. B. R. BANERJEE,J. J. IEAUSERand J. M. CAPENOS,Metal Sci. JI. 2, 76 (1968). 17. G. P. MILLERand W. I. MITCHELL,J. Iron Steel Inst. 208, 899 (1965). 18. S. FLOREEN and G. R. SPEICR, Trans. Am. Soe. &letaZs57, 714 (1964). 19. R. F. DECKER, J. T. EASH and A. J. GOLDMAN, Trtaw, Am. Soe. Meta.% 55,58 (1962).