The microstructure of class 350 maraging steel obtained by OM analyses is shown in Figs. 1 and 2 for the ST and STA samples respectively, allowing the observation of the surface characteristics in the ST condition, and the presence of lath martensite. The STA condition leads to an oxide microlayer with 2 ± 0,3µm formed at the samples surface.
The SEM-EDS analysis, presented in Fig. 3 and Table 2, indicated the segregation of Ni, Co, Mo and Ti from the base steel to the external sub-layer causing local enrichment near the layer boundary [28]. However, the semi-quantitative analysis by EDS presented in Table 2 indicates that the chemical composition of the bulk material was not affected by the heat treatment. In this sense, Klein et al.[17] stipulated that elemental oxidation in steam oxidized Fe-Ni-Co alloys can be explained by the iron diffusion mechanism. Since Ni and Co can’t be oxidized in the process, they serve as inert markers and their position indicates the interface between base material and oxidized layer.
Table 2: Cross Section and Surface top semi quantitative point chemical analyses of EDS in Wt%
Cross Section Analyses
|
Point Analyses
|
Fe
|
O
|
Ni
|
Co
|
Mo
|
Ti
|
1
|
68.0
|
27.0
|
0
|
2.5
|
2.4
|
0.0
|
2
|
60.6
|
27.4
|
4
|
3.4
|
3.5
|
1.1
|
3
|
50.5
|
25.6
|
7.8
|
6.8
|
7.5
|
1.8
|
4
|
49.8
|
23.3
|
8.7
|
8.0
|
8.1
|
2.2
|
5
|
35.7
|
6.0
|
31.7
|
19.15
|
5.5
|
1.8
|
6
|
32.2
|
7.1
|
32.2
|
20.66
|
6.1
|
1.8
|
7
|
48.3
|
3,2
|
26.0
|
15.78
|
5.3
|
1.4
|
8
|
58.5
|
1.9
|
19.7
|
13.02
|
5.49
|
1.41
|
Surface Analyses
|
Point Analyses
|
Fe
|
O
|
Ni
|
Co
|
Mo
|
Ti
|
1
|
65.6
|
31.7
|
0.9
|
1.1
|
0.5
|
0.1
|
The SEM images also allowed the measurement of the oxidized layer thickness, as observed in Fig. 3. It is important to note the existence of two distinct regions, one external and one internal sub-layer, with a total thickness of approximately 2 µm. The innermost layer presents diffusion behavior of the different alloying elements added to 350-grade maraging steel. These elements were involved in the formation of the protective oxide layer during thermal aging under superheated water vapor atmosphere [16]. In Fig. 5 and Table 2 the bulk material region near the boundary with the oxide layer, it is formed an intermediate layer, rich in Ni and Co in points 3 until 5, and point 6 and 7 showed a leading to austenite stabilization because Ni was increasing [21, 22, 29].
However, in Fig. 5 and Table 2, it is shown that the outermost layer formation follows a semi-qualitative stoichiometry of approximately 66% Wt of Fe to 32% Wt for O with traces of Mo, Ni and Co, indicating that the outermost formation is composed of hematite (Fe2O3) [14, 15]. This result was corroborated by Mössbauer spectroscopy on CEMS that confirms the presence of the sextet referring to the formation of hematite oxide, as presented in Fig. 6.
On the other hand, the Microabrasive wear testing characterization results shown in Fig. 7 presented the formation of two layers formed on the substrate. Following the V RUPETSOV and R MINCHEV method after 5 s of microabrasive wear testing, the outermost layer thickness measures approximately 1,5 ± 0,2 µm and the innermost layer one is about 0,7 ± 0,1 µm [30].
Hardness nano measurements were carried out at the spherical cap, at different depths, allowing to access the hardness profile as indicated by Figs. 7 and 8 with tree diferent layers, in top of surface until 0.8 µm the hardness is 1600HV, the second layer is in 0.8 µm until 1.5 µm the hardness is 2000 HV following with a gradual decrease in 1.5 µm until 1.8 µm with 1500 HV, than in the bulk depleted in iron and rich in nickel from 2.0 µm until 2,6 µm with 900 HV, and 2,6 µm is the bulk with 750 HV, average. The analysis of these regions means hardness values from the surface to bulk, presenting high standard deviation. The growth kinetics of oxides is non-linear, this behaviour is due to the fact that the atomic diffusion is not unidirectional, resulting in a non-planar boundary surface between substratemagnetite and magnetite-hematite, which leads to the high observed deviations. So, the initial measurements on the samples surface can be a hardness peak or a valley that characterizes the growth of the iron oxide layer under study. This high deviations indicates the existence of sub-layer interfaces, corroborating that the material presents a double layer formation, originated from the growth of the protective oxide during the heat treatment in a steam furnace.
Furthermore, the hardness measurements, accessed by nano indentation into the cap region, made it possible to observe average values for each separate layer: the white layer next to the substrate presented 900 ± 200 HV, the intermediate layer 2090 ± 380 HV, the region near the boundary 1640 ± 250 HV and the substrate 785 ± 120 HV. Nano-, micro- and impedance hardness results obtained on the surface and in the bulk aregathered in Table 3. In this sense, the impedance hardness measurements at the bulk region, in the ST condition, resulted in 442 ± 6 HV and 768 ± 6 HV for the STA condition. The oxidized surface presented a value of 830 ± 310 HV. It is clear that the surface measurements with nano and impedance techniques have a high deviation due to the porous characteristic of the outermost layer and these are techniques sensitive to heterogeneous surface formation [1, 5].
Table 3
Hardness measures with different techniques - HV
Conditions
|
Nano
|
Micro
|
Contact ultrasonic impedance
|
ST – bulk
|
399 ± 17
|
445 ± 25
|
442 ± 6
|
STA – bulk
|
772 ± 20
|
998 ± 47
|
768 ± 6
|
STA – top surface
|
790 ± 535
|
772 ± 20
|
826,04 ± 309
|
The element concentration profiles determined by GDOES are presented in Fig. 9. An oxide layer of about 1 µm is clearly visible, with oxygen content decreasing form 80 at.% to about 60 at.% and iron content increasing between 20 and 40 at.%. Ni, Co and Mo were not observed in this layer before ~ 0.7 µm, likely because of the rough interface between the top iron oxide and the underneath oxide. Below this iron oxide layer, the oxygen gradient is quickly decreasing till depth of about 2 µm whereas iron is still increasing till its bulk value. Within this intermediary layer located between 1 and 2 µm depth, Ni, Co and Mo are increasing till a maximum at 1.5 µm before decreasing back to their bulk value.. These profiles are confirming the growth mechanism of the oxide, based on iron diffusion toward the surface to build the Fe2O3 oxide, some inward diffusion of oxygen and then the relative enrichment in alloying elements (Ni, Co, Mo) in the intermediate oxidized depth due to the lower Fe content. [18, 31].
In order to obtain structural information about the surface layers, grazing incidence X-ray diffraction (GIXRD) was operated with different incidence angles to allow different penetration depths of the radiation. Figure 10 shows the diffractograms generated for incidence angles of 0.5, 1°, 1.5°, 2°, 3° and 5° [5, 32, 33], and Table 4presents the quantification data acquired by Rietveld method.
Table 4
Phases proportions obtained by Rietveld quantification method.
G. A °
|
Fe2O3
|
Fe3O4
|
γ
|
α
|
0,5°
|
65,5%
|
25,0%
|
8,8%
|
0,7%
|
1°
|
58,7%
|
29,1%
|
7,3%
|
4,9%
|
1,5°
|
57,6%
|
27,3%
|
12,5%
|
2,6%
|
2°
|
48,8%
|
34,8%
|
11,7%
|
4,6%
|
3°
|
45,8%
|
31,8%
|
15,2%
|
7,2%
|
5°
|
41,0%
|
22,6%
|
20,5%
|
15,9%
|
Using incident angles typically lower than 1.5°, the signal from the substrate can be minimized, increasing the intensity of the diffraction peaks associated with the crystalline structures next to the surface. Some researchers [24] argue that it is possible to obtain a more reliable quantification for the oxide layer using the relationship of photon interaction with the substrate thickness at some angles, especially in the case of phases with low volumetric fraction, as for example the intermetallic, binary and inorganic compounds formed at the substrate interface [2].
At the referred layer, the main crystalline phase is hematite, followed by magnetite. For the incident angles between 0.5° and 1.5°, an average hematite / magnetite ratio of 60% per 40% is maintained, which was also reported by other studies [14, 15]. However, for angles higher than 2°, the magnetite fraction increased, and at 3° the results presented also martensite peaks (charac teristic peaks of α’ Fe (110), (200) and (211)). From these results, it could be presumed that there was a formation of an external hematite layer and an internal magnetite sub layer. According to Rezek et al. [10], X-ray diffraction results indicated a higher percentage of hematite, inferring that a third oxide layer could be formed [2].
In an approach to calculate the penetration depth, it was used the method described by Birkholz [34], considering a sample with infinite thickness and the thickness of the upper layer that accounts for (1–1⁄(e) = 63%) of the measured intensity. With the thickness and phase quantification of each GIXRD diffractogram, an estimative of phase quantification for each thickness was done. Considering that only the depth penetration of the incident beam changes with the increase of α, the Eq. (2) was proposed to perform the layer phase quantification.
Where:
Q: Phase quantification measured in all volume by GIXRD
t: Analyzed film thickness
b: The surface area of analysis
q: Layer Quantification
n = 0,5°⟶5°
Figure 11 show the estimated results of the layer thickness on the material based on the Eq. 2. The result with 5° incidence angle shows a penetration depth of 3,5 µm, and the highest quantity of α and γ phases. This is in good correlation with the previously observed 2 µm thick oxide layer. Concerning the oxide layer, a first surface layer mainly composed of hematite is confirmed within the first 1 µm layer. Below, at the interface with the bulk, the magnetite is presenting a peak of proportion.
Graat et al. [35] made the analysis through the Fe 2p spectrum for a sample of pure Fe and obtained the peaks with binding energy of 706.8 eV for Fe0 and 709.8 eV and 711.2 eV for the Fe2+ and Fe3+ cations (Table 5). Satellite peaks present with a higher energy level, less intensity and always to the left of the main peaks with energy of 722.8 eV and 724.3 eV for Fe2+ and Fe3+ cations [32]. The doublets or multiplets that reveal the formation of satellite peaks in the spectrum of the main ions (Fe2+ and Fe3+). These peaks are due to the movement of electrons from the 3d orbital to the empty 4s orbital during the ejection of the electron photon from the 2p nucleus [35]. In analyses performed in Table 5the peaks summarize that binding energies used for XPS technique.
Table 5
Binding energies used for XPS analysis for the Fe 2p spectrum [33].
Espectrum Compound Fe 2p
|
Peaks of Binding Energies (eV)
|
Peak 1 (2p3/2)
|
Peak 2 (2p1/2)
|
Fe2O3
|
709,8–710,9
|
724,3
|
Fe3+ satellite
|
~ 719,0
|
~ 733,0
|
Fe3O4
|
709,0–710,4
|
722,0
|
Fe2+ satellite
|
~ 715,0
|
~ 730,0
|
FeO
|
708,4–709,4
|
N/A
|
Fe0
|
706,7–707,0
|
719,8
|
Fe 2p
|
710,9
|
724,5
|
FEOOH
|
711,8
|
-
|
In Figure 12 the XPS spectrum on the surface of the ST sample can be interpreted as the sum of the following iron components (Fe0, Fe2+, Fe3+ and Fe2O3) in the 2p spectrum and their respective satellite peaks. For the STA condition, Fe in hematite was identified at 709 to 710 eV at 2p3/2 and 722 to 724 eV at 2p1/2; Fe in magnetite is found at 728 eV for the 2p1/2 peak and in the range of approximately 713 to 718 eV for the 2p3/2 Peak. It is also observed the formation of satellite peaks to 2p3/2 Fe3+ at 714.5 eV , to 2p1/2 Fe2+ at 725 eV and to 2p3/2 Fe2+ at 716 eV. The 2p3/2Fe- in FeO is also found at 709.5 eV. In Figure 10, it can be seen that the analysis of the zero point (near the bulk-STA) at approximately 715 eV and 730 eV shows low presence of magnetite in the STA condition, as well as the peaks at 706.5 eV and 720 eV show the high presence of metallic Fe for the ST condition according [21, 33].
In Fig. 12 the XPS spectrum on the surface of the ST sample can be interpreted as the sum of the following iron components (Fe0, Fe2+, Fe3+ and Fe2O3) in the 2p spectrum and their respective satellite peaks. For the STA condition, Fe in hematite was identified at 709 to 710 eV at 2p3/2 and 722 to 724 eV at 2p1/2; Fe in magnetite is found at 728 eV for the 2p1/2 peak and in the range of approximately 713 to 718 eV for the 2p3/2 Peak. It is also observed the formation of satellite peaks to 2p3/2 Fe3+ at 714.5 eV, to 2p1/2 Fe2+ at 725 eV and to 2p3/2 Fe2+ at 716 eV. The 2p3/2Fe− in FeO is also found at 709.5 eV. In Fig. 10, it can be seen that the analysis of the zero point (near the bulk-STA) at approximately 715 eV and 730 eV shows low presence of magnetite in the STA condition, as well as the peaks at 706.5 eV and 720 eV show the high presence of metallic Fe for the ST condition according [21, 33].
The ST top in XPS analysis showed 41% of oxide composed of Fe2O3 in 709,96 eV and 723,27eV, 27% Fe metal formation in 706,78 eV e 720,14 eV, 7% FeO in 707,65 eV, and 16% other components. The top of STA formation of oxide composed of 63% Fe2O3 in 709,96 eV and 723,27eV and 37% of mixture of Fe3O4, FeO, FeOOH, Fe2+, Fe3+ and others is observed in 715,21 707,65, 711,58 eV. However, this analysis technique still needs to be improved, in Fig. 10 shows a movement of the peaks with the layer analysis, showing that the ratio of oxides formed changes with the depth, however the hematite and magnetite peaks divide the energy range very close, making the analysis difficult.
According to microabrasive wear and hardness analyzes, the layers have two characteristic thickness of approximately 1.08µm and 0.84µm, resulting in a 1.92µm thick oxide layer. Therefore, since the scanning of the spectra was carried out up to 1.8 µm, it was not possible to analyze the relative increase of magnetite and iron oxide in the deeper layers. However, it was noticed a decrease in the Fe2+ satellites peaks, which accompany the hematite phase, even though no peaks referring to magnetite were observed. It is also important to note that hematite was the main oxide composing all analyzed layers, showing a higher mass fraction at the surface, which decreased towards the center of the analyzed layer. This behavior was corroborated by XRD and GIXRD results and by the diffusion of iron and oxygen observed by GDOS technique. In brief, all presented techniques showed the formation of a triple oxide layer, composed at its surface majorly by hematite (Mossbauer), followed by a mixture of hematite and magnetite. Near the material’s bulk, it is also present a thin line with wustite and cobalt containing oxides, which leads to iron depletion and cobalt and nickel enrichment, favoring austenite stabilization and diffusion hardening at the matrix next the oxide layer.