NF709, a 20Cr-25Ni austenitic steel, falls in this class of novel alloys. It is manufactured by Nippon Steel and is currently regarded as one of the best austenitic steels for elevated temperature applications because of its creep and corrosion resistance.
The evolution of its microstructure during ageing at elevated temperatures is of considerable interest, both to ensure that no phase forms which is detrimental to creep properties and which could invalidate the extrapolations of short-term creep test data, and to identify any precipitates which might not occur in conventional steels or following short-term heat-treatments. NF709 has a composition which distinguishes it from the existing 20/25 austenitic stainless steels, as it contains a unique combination of carbon and nitrogen together with niobium and titanium.
Samples were sealed in quartz tube filled with argon and aged in
furnaces at 1023 and 1073 K.
Specimens for optical microscopy were electrolytically etched with a
solution of 10% (by mass) oxalic acid in distilled water for general
etching, and in a solution of 56 g / 100 ml KOH in distilled
water for outlining
-phase, according to the procedures
described in [4].
Thin foils for TEM (transmission electron microscopy) examination were electropolished using a solution of 5% perchloric acid in 2n-ethoxy-butanol, using a twin-jet electropolisher.
Bulk extraction was performed by dissolving the matrix electrolytically
with a solution of 10% HCl in methanol at 5-6 V. The residues were
then filtered with a membrane filter of 0.2
m pore
size. It was verified by prolonged centrifugation that no detectable
quantities of particles were left in the solution after filtration. X-ray
analysis was performed in a 2-
diffractometer.
The two materials in the as-received conditions had substantially different initial hardnesses and grain sizes (table 2). The X-ray analysis of extraction residues from the as-received samples showed further differences between the two steels. As indicated in table 3, NF709 does not seem to contain any Z-phase in the as-received state but instead contains substantial amounts of NbN. By contrast, NF709R does not show NbN but traces of Z-phase (CrNbN; a review of the different precipitates in creep-resistant austenitic stainless steels from one of the author has been published in [1]).
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These results are in agreement with SEM (scanning electron microscopy)
observations. TiN is present in both steels, in the form of
dispersed, coarse (up to 5
m) cuboidal particles as is often the
case for undissolved particles [1]. Nb-rich residual ( ie not dissolved during the solution treatment) particles are
smaller and have a less well defined shape (figure 1).
Because it was not clear whether the observed difference should be
attributed to different solution treatments or to chemical composition
variations, samples of both steels were solution treated 2 h at 1473
K. The alloys responded fairly differently, with NF709 showing
exaggerated grain growth and presenting a bimodal grain-size
distribution, while NF709R still showed a normal grain-size
distribution.
In both cases, the weight fraction of filtered residues was smaller
than in the as-received state. X-ray analysis did not reveal any
change in the nature of the phases present (see table
3), which were the same as for the
as-received samples. The new grain sizes are given in table
2.
To summarise, there is no doubt that the subtle chemical difference between NF709 and NF709R has important consequences for the microstructure. In particular, it is evident that Z-phase is a prominent feature of NF709R and it is likely that its presence at a solution treatment temperature as high as 1473 K results in a more uniform grain structure.
All the work reported henceforth focuses on the ageing of the industrially relevant as-received state rather than the resolution treated samples.
Specimens of NF709 and NF709R were aged for 1 h, 100 h (NF709) and 200 h at 1023 K. Extraction results (figure 2) show that the precipitation of M23C6 occurs during the very early stages of heat-treatment, although subsequent changes (figure 8) in the X-ray spectra of the residues indicate that it continues to evolve during ageing.
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The morphology and distribution of the precipitates varied between the two variants of NF709. Figure 3 shows optical micrographs of NF709 and NF709R aged 200 h at 1023 K. The intragranular alignment of precipitates observed in the 22Cr variant is not found in the 20Cr sample. Both steels show relatively intense precipitation on grain boundaries, incoherent twin boundaries, and, to a lesser extent, on coherent twin boundaries.
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M23C6 was found at numerous sites: strong presence on grain boundaries, with a globular morphology, on incoherent and coherent twin boundaries (ITB and CTB respectively) with a plate morphology, and around residual NbN precipitates. All these occurrences are well documented and have been reported on numerous occasions (for example, Lewis and Hattersley [6], Beckitt and Clarck [7], Singhal and Martin [8], Adamson and Martin [9]), with the exception of the formation of plates around residual NbX particles [1]. M23C6 has a cube-to-cube orientation relationship with the austenite, and its lattice parameter is three times that of the matrix; typical diffraction patterns appear as shown in figure 5 (d) and (f). After identification by diffraction and EDX (energy dispersive X-ray spectroscopy), it became evident that EDX fingerprints were sufficient to distinguish M23C6 and Z-phase.
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It is interesting to note the differences between the results obtained by X-ray analysis of extracted residues, and those obtained using TEM, particularly with regard to Z-phase. Although this phase is found with the latter, it was not detected using the former method. One of the possible causes is the size of the Z-phase precipitates. As can be seen in figure 4, these are seldom more than 50 nm in length after 200 h of heat treatment at 1023 K. This is significantly smaller than the 200 nm pore size of the membrane filter. To verify whether Z-phase particles were retained by the filter, the filtered solution was centrifuged. Since no deposit was found after prolonged centrifuging, it can be concluded that Z-phase was either dissolved or its quantity was too small to give a significant signal.
With this method, Z-phase is found in the as-received NF709R because it is present as residual particles, that is, coarse particles formed during solidification and undissolved by the solution treatment. By contrast, Z-phase formed during ageing was never found in the extracted residues. These observations are summarised in table 4.
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The same phases were identified in NF709R as in NF709. Figure 6 shows coarse M23C6 precipitates formed on the grain boundaries, in NF709R after 200 h at 1023 K. However, the aligned precipitates visible in figure 3 were identified as Z-phase and are therefore present in quantities significantly greater than in NF709. Also, the alignment observed (figure 6 (a)) does not occur in NF709. TEM investigation of thin foils of the as-received NF709R did not reveal an obvious difference in dislocation density. It is likely therefore that the alignment observed in NF709R is a consequence of the greater tendency for Z-phase formation in NF709R, so that dislocations lying along crystallographic directions rapidly become decorated with precipitates.
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The observations summarised in table 4
remain valid, although, as mentioned earlier, NbN and (Nb,Ti)C are not present,
while Z-phase is found as residual particles (typical size
1
m) and
precipitating with similar characteristics as above, but more densely.
Optical microscopy of NF709 aged 2500, 5000 and 10000 h for both heat-treatment temperatures showed that both the grain boundaries and incoherent twin boundaries were saturated with coarse precipitates. At 1023 K, incoherent twin boundaries were saturated only after 10000 h (this is shown in figure 7); globular intragranular precipitates were also visible at all times. At 1073 K, the intensity of precipitation was lower; this was particularly clear on the coherent twin boundaries which were relatively free of precipitates even after 10000 h. Most of the particles visible in optical microscopy correspond to the larger precipitates ( M23C6 and Cr3Ni2SiX), and it is therefore not surprising that precipitation appear more intense at 1023 K, approximately the temperature corresponding to the nose of the C-curve for M23C6 formation [1].
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While only M23C6 was identified in samples aged up to 200 h at 1023 and 1073 K, Cr3Ni2SiX was present in all samples aged for 2500 h and longer. This precipitate was found to occur at similar locations as M23C6, and to have a similar morphology, therefore making it difficult to distinguish the one from the other without compositional or careful diffraction analysis. Comparison between figures 2 (a) and (b) and figure 8 (a) and (b) illustrates clearly a significant increase in the amount of M23C6 (and Cr3Ni2SiX) when compared to TiN, as the ratio of the {333} M23C6:{200} TiN changes from about 1:2 (figure 2a) to 2:1 (figure 2b) and 10:1 (figure 8a and b).
Examination of the X-ray spectra of extracted residues, for 2500 h 5000 h and 10000 h at 1073 K, revealed a separation in the M23C6 peaks. As illustrated in figure 9 (a), this is true for the specimen aged at 1073 K but not at 1023 K where only a small shoulder is visible near the top of the peak.
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Table 5 presents the different lattice parameters measured for these ageing times. The lattice parameter measured for the diamond cubic phase, later identified as Cr3Ni2SiN is significantly greater than the one reported for Cr3Ni2SiC (1.062 nm, JCPDS 17-0330). The lattice parameter of Cr3Ni2SiN has not previously been published. The shoulder visible in figure 9 (a) is evidence that the lattice parameter of this phase, formed at 1023 K, is close to that of M23C6. This might be related to a composition change of Cr3Ni2SiX (where X refers to C or N): Williams [11] reported an increase in the Mo content of this phase with temperature (about 7 wt% per 100 K), which could explain the significant change in the lattice parameter. However our own measurements were not conclusively showing such a change of composition. Furthermore, attempts to confirm the absence of C and presence of N using Electron Energy Loss Spectroscopy were mostly unsuccessful, owing to the thickness of the Cr3Ni2SiX precipitates, the spectra did however indicate the presence of some N, but it was not possible to conclude as to the relative amounts of C and N.
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TEM examination of thin foils confirmed the presence of Cr3Ni2SiX whose composition matches reported values [11] (table 6); diffraction confirmed a lattice parameter close to 1.07 nm and the diamond-cubic structure.
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No other phases were identified during longer ageing treatments, although the existing phases had coarsen significantly (figure 11).
As shown below, the precipitation sequence for the NF709R version is different from that of NF709, in spite of their similar chemical compositions.
Optical micrographies were taken of NF709R aged 2500, 5000 and 10000 h at 1023 and 1073 K. When compared to NF709, the grain boundaries, incoherent and coherent twin boundaries appeared less densely decorated, in particular, the coherent twin boundaries were never outlined. At 1073 K, the grain boundary precipitates did not always form a continuous film, even after 10000 h.
After 2500 h at 1023 K, some intragranular plate-like precipitates of length up
to 5
m were found in most grains. After 5000 h, their density was
significantly larger, and their typical length between 5 and 10
m; some
coarse (3-5
m), globular particles were observed at some triple points and
occasionaly on grain boundaries (considerably larger than the precipitates
making up the continuous film decorating the boundaries). After 10000 h, these
plates were found in all grains and had lengths of up to 15-20
m, as
illustrated in figure 12(a).
After 2500 h at 1073 K, a few coarse grain boundary globular particles similar
to those described above were observed, but no intragranular plates.
After 5000 h, the latter were found only in the larger grains, with a lower
density than at 1023 K. After 10000 h, the globular precipitates appear more
numerous than at 1023 K; the intragranular plates were not visible in all grains
and were, in general, less numerous and shorter with typical lengths around 10
m, as illustrated in figure 12(b).
Therefore, while apparently showing a less dense carbides/nitrides precipitation than NF709, NF709R shows two kinds of particles not observed in the former (large intragranular plates and coarse globular triple points/grain boundary particles).
Both these new particles were identified, using SEM (figure
13), as
-phase, of composition close to 44Cr
40Fe 10Ni 6Mo, at%.
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As shown in figure 15, the separation is not as well defined as in NF709, and accurate lattice parameters could not be determined. However, two peaks are clearly overlapping, the one corresponding to the smaller lattice parameter this time being about half as intense as the other. This can be explained by the composition modifications presented by NF709R: the elements likely to control the amount of Cr3Ni2SiN such as Si or N are present in similar quantities, while the amount of C is halved, and as a consequence, the amount of M23C6 is reduced.
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Cr3Ni2SiN was found in similar locations as M23C6 (figure 14(b) and (c)). In addition, it was found as large intragranular plates (figure 16 (c)).
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The intragranular presence of
-phase only in large grains is
easily explained in terms of heterogeneous nucleation:
-phase
nucleation is easier on sites such as triple points and grain
boundaries. In grains of small sizes, the amount of surface for a
given volume is more than in large grains, and there is therefore
a greater number density of easy grain boundary nucleation sites for
-phase.
Because nucleation is more difficult within the grain, the tendency is
for
-phase to form intragranularly only if grain boundary
sites are not available, and if the driving force for nucleation is
large enough.
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Typical particle sizes tend to fall in three well separated categories: Z-phase
precipitates remain about 50-100 nm long;
M23C6 and
Cr3Ni2SiX are typically 0.5-1
m large; intragranular
-phase plates reach 15-20
m in length,
and grain boundary
-phase about 5-10
m. As noted earlier, residual
particles (NbN, TiN and (Nb,Ti)C) also tend to be coarse but are easily
identified because of their morphology and lack of orientation relationship, no
significant changes could be detected in the amount of TiN and (Nb,Ti)C.
Although
M6C is a quite frequently reported carbide in ferritic and
austenitic steels containing Mo, as
Fe3Mo3C,
the structure sometimes referred to as
encompasses a much wider
composition range [12] from
to
, where M
indicates a substitutional element such as Fe or Cr, while X indicates
an interstitial element such as C or N.
is a diamond cubic structure whose lattice parameter varies in the range
1.06-1.24 nm.
Cr3Ni2SiX is a particular composition of the
structure, whose lattice
parameter is 1.062 nm (JCPDS 17-330), which makes it extremely
similar to
M23C6 from a structural point of view, although the latter
is cubic while the former is diamond-cubic. Very few studies report
its presence under normal ageing conditions, while it is more
frequently found in irradiated austenitic stainless steels.
In 1981, Titchmarsh and Williams [13] reported Cr3Ni2SiC in FV548, a Nb stabilised version of type 316 stainless steel. In this steel, Cr3Ni2SiC is not found under normal ageing condition and its formation is attributed to the unusual segregation phenomena occurring in irradiated steels. In particular, point defect sinks are often surrounded by an increased amount of Si, because it is bound to the defects, and Ni, because it is slower than other elements to diffuse away from the sink. Both Titchmarsh and Williams [13] and Williams [11] assumed the carbon content of Cr3Ni2SiC. This is supported by the fact that G-phase, another Ni, Si rich phase of composition close to Ni16Nb6Si7 and space group Fm3m, forms instead of Cr3Ni2SiC in variants with a low level of carbon (0.02 wt%). A phase similar to Cr3Ni2SiC is reported by Jargelius-Pettersson [14] in a 20/25 N-bearing steel, but as a nitride rather than a carbide.
The substitutional content of Cr3Ni2SiC undergoes significant changes as the temperature of ageing is modified. Williams [11] reports increasing amounts of Mo and Fe substituting for Cr and Ni respectively, when the ageing temperature increases, and therefore proposed the more general formula (Cr,Mo)3 (Ni,Fe)2SiC. This latter study also gave evidence against the idea that Cr3Ni2SiC forms from M23C6 by infiltration of Ni and Si.
It is interesting to now study closely the precipitation of G-phase and
carbide during ageing of 20/25 steels.
The former phase is reported in various studies of 20/25-Nb stabilised
steels [15,16,17], while the latter
was only found in a 20/25 N-bearing steel, where it is a nitride, not
a carbide.
Powell et al. [15,16] and Ecob et al. [17] have
found G-phase in a 20/25 Nb stabilised steel, and observed that NbC
partially transforms to G-phase with time.
Ecob et al. [17] have related the increasing relative
instability of NbC compared to G-phase, in three different steels, to the
amount of oxygen present in the steels. To justify this observation, they
proposed that Si segregation was following oxygen segregation to the NbC
particles, therefore creating the thermodynamic conditions required for
the formation of G-phase. Nickel segregation may not be required in such
steels, since the Ni content is more than double that of AISI 316
stainless steel.
On the basis of these observations, it is possible to argue that G-phase is more stable than Cr3Ni2SiC in these steels: segregation provides the increased Si level required, while the dissolution of NbC is expected to raise locally the carbon level. Both phenomena are expected to be favourable to the formation of Cr3Ni2SiC, which is nevertheless not observed.
It seems therefore reasonable to say that if either phase was to be
found in NF709 or NF709R, it would be G-phase. However, none is
observed, while
Cr3Ni2SiN is present in significant quantities. In
a recent review by one of the authors [1], it has been
proposed that observations on the effect of nitrogen on the formation
of
M6C were better understood by considering
M6C and other
compositions as occurrences of the same
structure. Again, the
results here support the idea that the
structure is generally
stabilised by nitrogen, whether its composition is Mo-rich or Ni/Si-rich.
The difference between the ageing behaviour NF709 and NF709R is
noticeable given the
relatively small composition changes.
-phase formation is
favoured by both a high Cr and a low C content [1].
The presence of
-phase in NF709R but not in NF709 is
therefore not surprising.
The formation of copious amounts of
-phase caused great
concern about the ductility of aged NF709R, as a sharp reduction in toughness
and ductility is generally observed accompanying its formation. A simple
experiment was carried out to verify the deformation behaviour of the steels
provided: after ageing 10000 h at 1023 K, samples of both NF709 and NF709R
were deformed 30% in compression.
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Figure 17 shows that grain boundary cracking was observed at various places in NF709, but nowhere in NF709R. Moreover, the micrographs show that the intragranular plates can deform to a limited extent. This appear to be in agreement with reports of superior creep ductility in NF709R by Nippon Steel.
The impact of
-phase on the creep ductility is
not clarified, and while most tend to believe such a phase to cause a drop in
ductility, it has been suggested that this drop is a consequence of the overall
amount of carbides and nitrides [18].
The present observations support the fact that carbide and nitride precipitation in
general, rather than
-phase alone, causes the embrittlement in these steels.
The precipitation sequence of NF709 and NF709R have been studied for
heat-treatments of different durations at 1023 K and 1073 K. It
has been shown that, despite their similar chemical compositions,
these steels exhibit different precipitation behaviours. In particular,
there is evidence that the nitride CrNbN, known as Z-phase, is more
stable at higher temperatures in NF709R than in NF709. Also,
-phase is found in copious quantities in the latter but not in
the former.
With support of the existing literature, the formation of
Cr3Ni2SiN in
both NF709 and NF709R is taken as evidence that the
structure
is generally stabilised by nitrogen.
To verify whether the formation of
-phase was detrimental to
the mechanical properties, aged specimens were deformed, the results agreed with
data from Nippon Steel showing that NF709R exhibits superior ductility when
compared with NF709.
Different experimental techniques have been used together as it has
been demonstrated that each presents serious limitations in a
different domain of observation. In particular, X-ray analysis of extracted
residues, although a convenient technique for sampling large quantities of
material, is shown to be of limited interest for small (
nm) particles,
as it cannot detect most of them.
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