Microstructural Characterization
Figure 1 shows dilatations of the high-Si hypereutectoid bearing steel during holding at different temperatures. The transformation finished after holding at 250, 300, and 350 °C for 30, 8, and 5 h, respectively. However, the dilatometric amount in length induced by isothermal transformation increased with the decreasing transformation temperature, ensuring the transformation was finished. This implies that the deceleration of transformation kinetics is related to the decrease in transformation temperature. Figure 2 shows the microstructural evolutions of the high-Si hypereutectoid bearing steel transformed at 250, 300, and 350 °C. After the transformation finished, the microstructure mainly consists of needle-type bainite and retained austenite (RA) with block morphology, as shown in Fig. 2b, d, and f. However, after the partial transformation, the microstructure includes bainite, RA, and some martensite, as shown in Fig. 2a, c, and e. The experimentally determined martensite start temperature (M
s) at a rate of 20 °C/s after austenitizing at 1100 °C for 15 min and then isothermal transformation at different conditions is listed in Table 2. It indicates that the experimentally determined M
s is reduced as compared to that during directly quenching at a rate of 20 °C/s (120 °C), implying that the isothermal transformation of austenite contributes to the thermal stability of untransformed austenite improved.
Table 2 Experimentally determined M
s (°C) at a rate of 20 °C/s after austenitizing at 1100 °C for 15 min and then isothermal transformation at different conditions
Figure 3 shows the SEM and TEM micrographs of the high-Si hypereutectoid bearing steel transformed at 250, 300, and 350 °C for 12 h. The microstructures mainly consist of bainitic ferrite plates and RA with block and film morphology. Gong et al. [26] suggested that short-range diffusion of carbon atoms from bainitic ferrite plate to austenite film occurs. Hence, two populations of austenite with different carbon concentrations exist. It should also be emphasized that the TEM image (Fig. 3b) confirms the absence of precipitation at ferrite/austenite boundaries. Thus, it infers carbide precipitation is significantly suppressed during the isothermal transformation. As indicated by previous investigators, this results from the presence of Si, which leads to suppressed cementite precipitation in steels [27]. This is generally explained by the fact that the cementite, when it forms under paraequilibrium conditions, traps the Si as it grows. The resulting reduction in the free energy change of the reaction slows down the kinetics of precipitation. The cementite can then only form with the partitioning of Si [28]. Thus, it is suggested that the addition of 1.3 wt.% Si to hypereutectoid bearing steel suppresses the precipitation of carbide during bainite transformation. These results demonstrate that the bainite transformation during holding at 250–350 °C has incomplete transformation phenomenon, which is defined as the temporary cessation of bainitic ferrite formation before the fraction of austenite transformed to ferrite, allowed by the lever rule in the absence of carbides precipitation at ferrite/austenite boundaries, is reached [29].
RA carbon content (wt.%) and its fraction (vol%) determined by XRD analysis in the high-Si hypereutectoid steel transformed at different temperatures, ensuring the transformation was finished, are listed in Table 3. It is clear that the extent of transformation is a sensitive function of temperature and this is totally characteristic of the incomplete transformation phenomenon. The volume fraction and carbon content of the RA gradually decreased and increased with the transformation temperature reduced, respectively. In the suppression of carbide precipitation, however, a simple mass balance estimate of the carbon suggests that the carbon content of bainitic ferrite should be significantly higher than the paraequilibrium value during bainite formation at low temperature.
Table 3 RA carbon content (wt.%) and its fraction (vol%) determined by XRD analysis in the high-Si hypereutectoid bearing steel transformed at different temperatures, ensuring the transformation was finished
Bainite Transformation Characteristic
In order to analyze the crystallographic orientation relationship (OR) between bainite and its parent austenite, the possible ferrite/austenite OR was applied. Table 4 shows the possible ferrite/austenite OR, including Kurdjumov–Sachs (K-S), Nishiyama–Wassermann (N-W), Pitsch and Bain ORs [30, 31]. Figure 4 shows the inverse pole figure (IPF) maps of bainitic ferrite (bcc) and austenite (fcc) and the OR maps of the interfaces between bcc and adjacent fcc in the high-Si hypereutectoid bearing steel transformed at 250, 300, and 350 °C. The tolerance angle in this analysis was set as 3°. The IPF images of bcc, as shown in Fig. 4a1, a2, and a3, clearly reveal that each bainitic ferrite sheaf has one single crystallographic variant, although it is possible to observe more than one variant within a single austenite grain. Remarkably, the OR of the interfaces between bcc and adjacent fcc is close to the N-W and K-S ORs, which is indicated by red and blue lines shown in Fig. 4c1, c2, and c3, respectively.
Table 4 Possible orientation relationship (OR) between austenite (γ) and ferrite (α) [30, 31]
Figure 5 shows the TEM dark-field images on bainitic ferrite and austenite together with selected area diffraction pattern (SAD). SAD in Fig. 5c and dark-field images taken from bainitic ferrite and austenite in Fig. 5a and b, respectively, indicate (110)α//(111)γ and [\( 1\bar{1}\bar{1} \)]α//[\( 1\bar{1}0 \)]γ, which is descried as K-S OR [30, 31]. Therefore, the isothermal transformation of austenite at 250–350 °C is inferred to be bainitic and take places by the displacive (diffusionless) mechanism. Again, experimental results on the temporary cessation of bainitic ferrite formation in high-Si hypereutectoid bearing steel confirm that the incomplete transformation phenomenon can be explained in terms of the diffusionless growth of bainitic ferrite subunits. In addition, carbon enrichment in the untransformed austenite occurs immediately after the bainitic ferrite formation. In the suppression of carbide precipitation from austenite, carbon enrichment in RA, as shown in Table 3, is a manifestation of the formation of bainitic ferrite with a full supersaturation of carbon followed by carbon partitioning between bainitic and austenite. However, the driving force for the formation of bainitic ferrite plates decreases as the carbon concentration in the untransformed austenite approaches a value, at which the free energy of ferrite and austenite phases of the same composition become identical, resulting in the displacive transformation becomes thermodynamically impossible [11].
The dislocation density of bainitic ferrite formed at 250, 300, and 350 °C was calculated to be 4.1 × 105, 3.5 × 105, and 2.0 × 105 m−2, respectively. The relatively high dislocation density within bainitic ferrite is often attributed to the fact that the shape deformation accompanying the displacive transformation is accommodated at least partially by plastic relaxation [32, 33]. According to the tempering theory of Kalish and Cohen [34], however, carbon atoms are energetically favorable to remain segregated at dislocation compared with their partitioning into surrounding austenite or their presence in the carbide lattice. Hence, if the dislocation density within bainite ferrite is high, sufficient carbon can be captured by dislocation. Atom probe tomography results reported [35] elsewhere revealed that a substantial quantity of carbon (7.4 at% C) was trapped at dislocations in the vicinity of the ferrite/austenite interface in NANOBAIN steel. These results indicate that the bainite ferrite formed at lower temperature has higher carbon content. Thus, it is demonstrated that despite the significant fraction of bainite formed at 250 °C, the RA does not seem greatly enriched in carbon compared to that at 350 °C.
Effect of Si on the Deceleration of Bainite Transformation
Figure 6 shows the bainite transformation kinetics of the high-Si hypereutectoid and AISI 52100 bearing steels during holding at 300 °C. The transformation kinetics of the high-Si hypereutectoid bearing steel is much more sluggish compared to that of the AISI 52100 bearing steel. This implies that the bainite transformation is obviously decelerated by the addition of 1.3 wt.% Si in hypereutectoid bearing steel, consistent with the results presented in Ref. [36]. Figure 7 shows the SEM morphology of the AISI 52100 bearing steel transformed at 300 °C. The microstructural image reveals that carbide can significantly precipitate and austenite decomposes into ferrite and carbide during holding at 300 °C. However, the incomplete transformation phenomenon is not well pronounced in the AISI 52100 bearing steel, where carbide precipitation dominates.
Carbon enrichment of austenite leads to the precipitation of carbides which implies that the effective carbon enrichment of austenite is negligible. However, in the high-Si hypereutectoid bearing steel, the carbide precipitation is kinetically suppressed, leading to significant carbon enrichment of austenite associated with the carbon partitioning after bainite formation. Accordingly, once Si exerts a suppressing effect on the carbide precipitation in austenite, the formation of bainitic ferrite will lead to carbon enrichment of austenite adjacent to the ferrite plates. The higher carbon content of austenite lowers the driving force for the subsequent formation of ferrite plates, and the sympathetic nucleation rate of ferrite decreases [37]. The experimental result confirms that the deceleration of bainite transformation kinetics of the high-Si hypereutectoid bearing steel is related to the suppression of carbide precipitation from austenite. Therefore, the suppression of carbide precipitation is also interpreted as one of the necessary conditions for manifestation of incomplete transformation phenomenon because the consumption of carbon atoms to form carbides makes carbon enrichment in austenite difficult, and thus cessation of bainitic ferrite formation is also difficult.