3.1. Microstructural Evolution
Figure 1a-d shows the OM of the four strain samples before impact,
Figure 1e-t illustrates the OM of the four AZ31 samples following impact at various strain rates. The evolution of the impacted samples can be categorized into four stages as the strain rate increases. (1) Strain rate of 800 s
-1: a significant amount of twins form across all samples. (2) Strain rate of 1400 s
-1: the previously formed deformation twins largely disappear, and further impact leads to grain size reduction. (3) Strain rate of 2000 s
-1, the impacted specimen experiences further growth in grain size accompanied by a noticeable rise in temperature. (4) Strain rate of 2400 s
-1, all samples undergo fracture, characterized by a prominent presence of adiabatic shear bands and deformation twins within the sample. Clearly, the extent of temperature rise is positively correlated with the magnitude of the strain rate [
16,
29,
30], which in turn, the coarsening of grain size can be imaged.
Figure 2a-d presents the inverse pole figure (IPF) and grain size distribution diagram of samples that underwent different rolling reductions after impact at a strain rate of 2000 s
-1. The impact-induced grain structure of the R0 and R30 appears relatively uniform, while the R10 and R20 exhibit significant variation in grain size. In particular, the maximum grain size observed in the R10 is approximately 14.5 times larger than the average grain size (AGS). This discrepancy can be attributed to two factors. On the one hand, the short impact deformation time results in some grains failing to promptly coordinate deformation, leading to significant disparities in grain distribution. On the other hand, the initial grain homogeneity also influences this phenomenon. It is important to highlight that irrespective of the AGS before impact deformation, the AGS of each sample converges to around 9 μm after impact at a strain rate of 2000 s
-1. Even when the morphology varies considerably among all samples, the impact-induced deformation facilitates the formation of numerous fine grains within the coarse grains, enabling coordinated deformation and a remarkable reduction in AGS. This findings aligns with observations from previous dynamic impact studies on Mg alloys [
31,
32,
33].
Figure 3 shows the texture distribution of the samples after impact at a strain rate of 2000 s
-1. There are no significant variations of texture intensity. The (0001) pole figure (PF) demonstrates a predominantly parallel distribution in relation to the impact direction (ID). Additionally, an IPF reveals the formation of a non-fiber texture component that is roughly parallel to the transverse direction (TD). In addition, the texture components were also detected transitional orientations between the [10-10]∥TD and [11-20]∥TD.
During high-speed impact on Mg alloy, a considerable number of deformed grains are formed to accommodate the severe deformation [
34].
Figure 4 presents the distribution and proportion of grains below the AGS in the impacted samples, along with their corresponding textures. The volume fraction (
Vf) of grains below the AGS is approximately 13%, and highly uneven grain distribution can be found due to more unbreak coarse grains when comparing with
Figure 2. Wang et al. [
35] observed that when the compression direction (CD) aligns with the rolling direction (RD), the texture would be enhanced. Conversely, when the CD is perpendicular to the RD, the texture becomes weaker.
The corresponding (0001) PF reveals that while certain grains maintain the orientation distribution with the c-axis parallel to the impact direction (ID), most grains tend to diffuse along the normal direction (ND) and form orientations offset by about 30° along the transverse direction (TD). The color distribution in the figure shows that the texture formed after impact becomes more pronounced as the rolling reduction increases. Weak texture components are observed in R0 and R10 samples, while R20 and R30 specimens exhibit distinct base poles. This illustrates that when the two deformations share the same direction, the deformation during the initial process also influences the texture generated by the subsequent deformation.
Generally, the deformation twins obseved at high strain rates directly contributes to an increase in the average orientation difference (known as KAM), as depicted in
Figure 5. The impacted samples display remarkably high KAM values, and the distribution of KAM within the coarse grains exhibits notable heterogeneity. This phenomenon can be attributed to two factors: (1) the very short impact process limited the ability of some coarse grains to promptly undergo coordinated deformation. As a result, non-uniform strain emerges within these grains. (2) a multitude of small grains involving dynamic recrystallization (DRX) forms within the coarse grains subsequent to impact. These newly-formed grains exhibit relatively low KAM values and actively contribute to coordinating and influencing the KAM distribution to a significant extent. A similar finding was observed by Deng et al. [
38], where they proposed twinning promotes the generation of slip to further achieve coordinated deformation. Thus, a substantial number of twins are indeed produced during the impact process to facilitate coordinated deformation, resulting in a reduction in the AGS.
In addition, the microstructure of the samples after impact predominantly contains tensile twins, while compression twins and double twins are nearly absent. These tensile twins are primarily observed within the coarse grains, which highlights that tensile twins dominate the initial twinning deformation at high strain rates, as suggested by Chen et al. [
39].
Figure 6 illustrates the specific distribution and
Vf of twins in specimen. For instance, in case of the impact samples at a strain rate of 2,000 s
-1, the R20 specimen exhibits the highest number of tensile twins, with a
Vf of 23.4%. The formation of tensile twins mainly arises from certain original grains with basal texture. Additionally, due to the low Critical Resolved Shear Stress (CRSS) value associated with activating tensile twins, the strains corresponding to the impact deformation stage are fully sufficient to induce the highest number of tensile twins.
Comparing the IPF in
Figure 2, nearly all the tensile twins form within grains tend to exhibit a distribution aligned with the [11-20]∥TD, as illustrated in
Figure 4. However, the actual orientation of the twins exhibits a noticeable deviation from this direction. As a result, the texture with a higher quantity of formed twins after impact significant weakening in the [11-20]∥TD. Furthermore, it is notable that in
Figure 4e, no non-fiber texture parallel to the TD forms. Gao et al. [
40] also discovered that twins not only reduce the intensity of the texture but also alter the type of texture. In addition, the formation of numerous tensile twins within specific coarse grains has largely affected the neighboring grain orientations. To conduct a comprehensive analysis, we focused on grains within two typical designated green rectangular frames in
Figure 6. The details are presented in
Figure 7, using “P” to denote the parent grain and “ETs” to represent the tensile twins.
In region A, a considerable number of tensile twins are observed within the P1 grains, and their orientations are generally consistent with the grains below the AGS. The corresponding texture components are formed near a 30° deviation from the ND to the TD in the (0001) PF. Conversely, the orientations of the grains surrounding P1 differ significantly from P1 itself. Some grains exhibit texture components similar to those of the tensile twins, while others align with the [10-10]∥TD. Particularly, the black rectangular frame in
Figure 7a reveals compelling evidence of the influence of tensile twins on the orientation of surrounding grains. A discernible gradient trend is observed in the grain boundary (GB) orientation difference among the three small grains formed adjacent to the twins. Moreover, the colors of these grains undergo significant changes. These observations further emphasize that the formation of tensile twins substantially impacts the orientation changes of the surrounding grains [
41,
42].
In region B, a number of tensile twins are also formed within the P2 and P3 grains. However, unlike the twins in region A, only a few grains surrounding the parent grains of these twins exhibit similar orientations. The texture orientations of the majority of grains align with the [10-10]∥TD, with only a small number of grains sharing a similar orientation to their parent grains. Notably, it is important to highlight that grains with significantly different orientations form at higher twin densities within the P2 grains. The texture orientations of the small grains formed around these grains closely resemble their own orientations, differing from the P2 grains. These observations indirectly indicate a notable influence of the formation of tensile twins on the texture components of the surrounding grains.
3.2. Mechanical Property
Figure 8 presents the true strain-stress curves of gradient rolling samples with varying deformations after impact at different strain rates. All curves exhibit an S-shaped plot, which is characteristic of the twinning-dominated deformation mechanism in Mg alloys [
43]. This kind of deformation process can be divided into three stages. Initially, during the early stage of impact, the alloy undergoes significant work hardening, with the stress rapidly increasing as strain accumulates. Once a certain threshold of strain is reached, a distinct yield platform becomes evident, and the stress exhibits a gradual upward trend. The presence of a low yield platform arises from the loading direction induced by impact, favoring the formation of tensile twins in the initial stages of deformation. The relatively low CRSS required for tensile twin formation allows the material to adjust its deformation by generating such twins, leading to an earlier attainment of the yield condition. As deformation progresses further, the stress continues to rise but the material experiences a competition between strain hardening and adiabatic temperature rise associated with high strain rates deformation. This competition results in fluctuations in the curve, leading to an oscillating behavior [
44]. And the stress reaches its peak value. Subsequently, the stress gradually decreases until deformation ceases.
Figure 8e represents the true strain-stress curve under quasi-static compression. It can be observed that the shape of the curve is similar like previous
Figure 8a-d but the fluctuation region at the peak is absent, which indicates that there is no pronounced adiabatic temperature rise. Additionally, the peak stress is reduced, suggesting that higher strain rates contribute to work hardening.
Figure 9 illustrates the yield strength (YS) and peak compressive strength (CS) of all specimen in
Figure 8. The R20 sample exhibits a higher YS compared to the other samples. Specifically, at a strain rate of 1400 s
-1, the YS of the R20 sample reaches 175 MPa, surpassing the YS of the R0 sample at a strain rate of 0.001 s
-1 by 65 MPa. In case of the peak CS within the range from 0.001 s
-1 to 2000 s
-1, the CS increases with higher strain rates. However, the impacted samples fractured when the strain rate reaches 2400 s
-1, resulting in a significant decline in CS. Notably, the R20 sample consistently exhibits the highest CS across all strain rates. For example, the CS reaches 644 MPa at a strain rate of 2000 s
-1, exceeding the CS of the same strain sample at a strain rate of 0.001 s
-1 by 145 MPa. This also emphasize the pronounced sensitivity of the CS of the impacted samples to the strain rate [
30,
45].
Generally, the mechanical properties can be strengthened by solid solution strengthening, grain boundary strengthening, dislocation strengthening, and shear band strengthening [
46,
47,
48,
49]. The TEM characteristics was carried out for better understanding for such strengthening machinsm.
Figure 10a displays the formation of high-density dislocations in the sample after impact, which agrees well with
Figure 5 demonstrating numerous dislocations at high strain rates from KAM analysis. Furthermore, the presence of layered structures in the dislocation region (see
Figure 10b) and lattice distortions in the high-resolution image (see
Figure 10c) confirm the existence of stacking fault (SF) resulting from the interaction between SFs and a large number of dislocations. This interaction severely hinders the plastic deformation process, thereby improving the YS [
50,
51]. Additionally, twin-twin interaction is observed within the impact specimen (see
Figure 10d, e), which also contributes to strengthening of AZ31 alloy. In addition to dislocations and twinning,
Figure 10g reveals the presence of numerous nano-scale second-phase particles and some DRXed grains. Detailed EDS mapping indicates these second particles to be Al-Mn phases. Most of these particles are located near dislocations and hinder the movement of dislocations to some extent, thus enhancing the properties as well. Besides, companied with
Figure 2 exhibited lots of fine grains, a decrease in grain size by DRX enhances the YS according to the well-known Hall-Petch equation. In case of quasi-static compression with low strain rates, the YS and CS of as-rolled sample remain low. However, when the strain rate reaches a medium level and the sample still does not fractured after impact, both the YS and CS increase significantly (i.e., R20 sample). When the strain rate reaches high level that causes specimen failure, the corresponding strength decreases dramtically, and the alloy exhibits negative strain rate sensitivity.
Figure 11 illustrates the Vickers hardness of AZ31 alloys subjected to different rolling reductions after impact. By examining the OM presented in
Figure 1 and correlating it with these hardness values, it becomes apparent that the hardness values of all samples increase significantly with higher strain rates. However, at strain rates of 1400 s
-1, 2000 s
-1, and 2400 s
-1, the hardness values do not exhibit a positive strain rate sensitivity. Specifically, both the R0 and R30 samples consistently exhibit hardness values of approximately 70 HV after impact. In contrast, the hardness values of the R10 and R20 samples demonstrate a negative strain rate sensitivity with an increase in strain rate from 1400 s
-1 to 2000 s
-1. This phenomenon is attributed to the significant increase in grain size observed in the R10 and R20 samples following impact at a strain rate of 2000 s
-1. It is noteworthy that despite all samples fracturing at a strain rate of 2400 s
-1, the hardness measurement on the fractured sample indicates that the hardness value remains higher than the value prior to impact. This suggests that a substantial amount of deformation energy was absorbed by the sample prior to fracture failure. Moreover, it is worth emphasizing that
Figure 11 exhibits a significant hardness errorbar in shardow for the R10 sample following impact at a strain rate of 2400 s
-1. Correlating it with the OM shown in
Figure 1n, it becomes evident that the microstructure of the sample becomes highly heterogeneous after impact, primarily due to the presence of numerous shear bands. These measurements further support the well-established Hall-Petch relationship between hardness and grain size [
53].
Further examination of the shear band are presented in
Figure 12. It is observed that although the grains within the shear band remain unevenly distributed, their size is significantly smaller compared to previous structures. Additionally, some nanocrystals and numerous nano-scale second phases in the shear band as depicted in
Figure 12b, d contributing to the improved performance. However, at high strain rates, the occurrence of molten metal can be seen in
Figure 12d indicated by the red arrow, which due to the local generation of heat during impact, resulting in limited heat dissipation and elevated temperatures within the shear band. Moreover,
Figure 12b,d highlight the presence of micro-cracks surrounding specific grains, as indicated by the orange arrows. These micro-cracks have a tendency to propagate along adiabatic shear bands and can act as precursors to failure [
54,
55], providing an explanation for the fracture at the strain rate of 2400 s
-1.
In summary, when the as-rolled AZ30 alloy is subjected to high strain rates deformation, a substantial number of deformation twins are generated, leading to an increase in dislocation density and noticeable work hardening. Concurrently, shear bands form as dislocations slip along specific GBs, resulting in the accumulation and interaction of dislocations, thereby enhancing the final performance. Moreover, due to the limited dissipation of heat, there is a rapid rise in temperature during short impact, leading to grain recrystallization, occurrence of molten metal and enhanced work hardening. All these factors contribute to a reduction in the AGS and an improvement in the mechaincial properties. Additionally, the continued development of adiabatic shear bands is accompanied by the formation of cracks, which lead to the failure and fragmentation of alloys at excessively high strain rates.