Fracture surfaces of uncharged specimens were analyzed and compared with those of their hydrogen-charged counterparts using a Thermo Scientific AXIA ChemiSEM scanning electron microscope (SEM) (Waltham, MA, USA) equipped with energy dispersive X-ray spectroscopy (EDX) capabilities. The findings have been discussed in the subsequent sections.
5.1. Uncharged Specimens
Analysis of the fracture surfaces of the uncharged 44W steel subjected to uniaxial tensile loading is presented in
Figure 10. As shown in
Figure 10a, the three distinct regions highlighted and color-coded showed various features. Region 1 (red) revealed the presence of inclusions along with evidence of ductile failure through dimpling. Region 2 (yellow) exhibited signs of directional cracking, indicative of localized stress concentration and crack propagation. Region 3 (blue) was characterized by stretched dimples and microvoids, features typically associated with plastic deformation and void coalescence mechanisms.
The dimples and microvoids (
Figure 10b,d) are indicative of expected ductile fracture mechanisms, which typically occur when the material undergoes significant plastic deformation prior to fracture. This deformation initiates at stress concentration points, such as inclusions or second-phase particles within the microstructure, leading to microvoid nucleation. These microvoids grow and coalesce under tensile stress, forming the characteristic dimpled appearance on the fracture surface.
The directional cracks observed (
Figure 10e) are a result of localized stress intensification within the material, where the primary cracks propagate along paths of least resistance. These paths are often aligned with areas of microstructural weakness, such as inclusions or interfaces between phases, which act as crack initiation and propagation sites.
The inclusions identified on the fracture surface (
Figure 10b,c), through EDX analysis (
Table 5), presented additional interpretations into their elemental composition and role in the fracture process. The high silicon content at point 1 (
Figure 10c) suggests the presence of silicon-containing inclusions, such as silica (SiO
2) and silicates (e.g., MnSiO
3, Fe
2SiO
4). The former commonly forms during steelmaking as a result of oxidation reactions involving silicon when it reacts with oxygen through solidification or refining, and the latter forms when silicon reacts with other elements like manganese (Mn), iron (Fe), or calcium (Ca) during the steelmaking process [
102,
103,
104]. Such inclusions are often brittle and act as stress concentrators, facilitating the nucleation of microvoids and crack initiation under tensile loading [
50,
51].
Point 2 (
Figure 10c), characterized by high Fe content, is identified as a ferritic region within the matrix. This area represents an iron-rich phase with minimal alloying element segregation, likely where the matrix remains relatively pure. While such ferritic regions are generally less susceptible to fracture initiation, they may still influence crack propagation by interacting with surrounding inclusions.
The fracture surface of uncharged Monel 400 (
Figure 11) subjected to uniaxial tensile testing was also analyzed. As shown in
Figure 11a, region 1 (red) displayed coalesced microvoids and dimples, which are typical indicators of ductile fracture mechanisms. Region 2 (yellow) revealed the presence of microcracks and scattered microvoids, suggesting localized initiation sites for fracture propagation. Region 3 (blue) exhibited slip regions and fibrous dimples, reflecting plastic deformation and a fibrous fracture texture associated with the material’s toughness.
Shear lips (
Figure 11a) form near the edges of the fracture surface due to shear stresses that dominate in these regions, resulting in localized plastic deformation. This is characteristic of a mixed-mode fracture where both tensile and shear forces contribute to failure. Dimples and fibrous dimples (
Figure 11b,c), further indicative of ductile fracture, result from the nucleation, growth, and coalescence of microvoids, as explained above. However, as voids grow under tensile stress, they eventually merge, forming a fibrous appearance in the fracture surface, especially in regions of extensive plastic deformation.
Slip regions (
Figure 11c) evolve from localized plastic deformation due to dislocation movement along specific crystallographic planes under the applied tensile stress. These regions appear relatively smoother and are associated with areas of intense deformation. Microcracks are initiated at stress concentrators such as inclusions, grain boundaries, or other defects within the material and propagate as the applied stress exceeds the material’s fracture toughness, and their growth is often influenced by the microstructural characteristics of Monel 400.
Coalesced microvoids (
Figure 11b,d), as explained above, result from merging voids as the material encounters further plastic deformation. This coalescence marks the final stage of ductile fracture, where the material fails as a result of the complete loss of load-bearing capacity in the deformed region.
The fracture surface of the uncharged 304L austenitic stainless steel subjected to uniaxial tensile testing is displayed in
Figure 12. As shown in
Figure 12a, region 1 (red) revealed coalesced microvoids, micropores, elongated voids, dimples, and a visible crack direction, features indicative of ductile fracture accompanied by localized plastic deformation. Region 2 (yellow) showed a concentration of dimples and voids, further supporting the ductile nature of the fracture in that area. Region 3 (blue) identified the crack origin and the direction of its propagation, offering detailed comprehension of the initiation site and fracture path.
The presence of elongated dimples (
Figure 12b) observed on the fracture surface of uncharged 304L austenitic stainless steel subjected to tensile loading, alongside other fracture characteristics (
Figure 12c,d) already discussed, reflects the ductile nature of the material under the given loading conditions. Elongated dimples are indicative of crack initiation and microvoid coalescence, which are common features of ductile fracture, where the shape and orientation of the dimples correspond to the direction of plastic deformation experienced during tensile loading. Mechanistically, this phenomenon begins with the nucleation of microvoids at the aforementioned stress concentrators present in the material. As the tensile stress increases, these voids grow and elongate in response to the applied load, with the elongation direction aligning with the principal tensile axis. This morphology is a result of the high degree of plastic strain sustained by the material before the final fracture, indicative of significant energy absorption during deformation.
The fracture surface of the uncharged arc-DED 308L austenitic stainless steel (
Figure 13) subjected to tensile loading reveals a complex relationship of deformation and failure mechanisms, as evidenced by the fibrous dimples, very large voids, and stream-like markings. These features collectively highlight the material’s ductile response under tensile stress, while also pointing to microstructural inhomogeneities and anisotropic properties fundamental to the AM process. The mechanisms of some observed features, i.e., shear lips and fibrous dimples (
Figure 13a,b), are as discussed above.
The very large voids observed (
Figure 13c,d) on the fracture surface likely originate from the inherent characteristics peculiar to the AM process. In AM-manufactured materials, incomplete fusion, trapped gas, or uneven solidification can create larger voids within the microstructure [
105,
106]. Under tensile loading, these voids act as stress concentrators, growing disproportionately as the material deforms plastically. Their size and prominence suggest they play a significant role in the fracture process, as they reduce the load-bearing cross-sectional area and promote early void coalescence.
The stream-like markings reflect the directional nature of plastic flow during tensile deformation. These markings likely result from the alignment of microstructural features and localized stress gradients, guiding the flow of material as voids grow and coalesce. This directional texture is accentuated in AM materials due to the layer-by-layer nature of the deposition process, which introduces anisotropy and preferential deformation paths. Together, these features paint a comprehensive picture of the interplay between the AM microstructure and the ductile failure mechanisms activated under tensile stress.
5.2. Charged Specimens
To effectively evaluate and delineate the potential effects of hydrogen permeation on material behavior, a comparative analysis was conducted between the fracture surface features of uncharged specimens and those subjected to the highest levels of hydrogen charging (1.30 wppm). This approach enabled a clear distinction between the baseline fracture characteristics and the alterations induced by maximal hydrogen ingress, providing critical insights into the embrittlement mechanisms and microstructural responses associated with hydrogen exposure. The fracture surface of 44W steel subjected to 1.30 wppm hydrogen content cathodic hydrogen charging (
Figure 14) exhibited distinct features: cleavages, quasi-cleavages, microcracks, river marks, transgranular cracks, and sharp edge ridges that are significantly influenced by the presence of diffused and dissolved hydrogen. In contrast to the ductile features like dimples, microvoids, and shear lips observed in uncharged specimens, these brittle fracture characteristics are a direct consequence of HE, where the diffusible hydrogen weakens the steel’s microstructure, making it more susceptible to brittle failure.
The formation of sharp edge ridges (
Figure 14a) is indicative of severe localized strain near crack tips, where hydrogen has embrittled the material, reducing its ability to undergo plastic deformation and leading to the formation of sharp, brittle fracture features. Also, river marks (
Figure 14b), typically associated with ductile fracture, were also present but less pronounced in the hydrogen-charged specimens. In the presence of hydrogen, these river marks can become irregular or even suppressed due to the brittleness of the material caused by HE. This transition from ductile to brittle behavior is a direct manifestation of the detrimental effects of hydrogen diffusion, where the material’s ability to undergo plastic deformation is significantly reduced.
The formation of a directional crack mechanism in hydrogen-charged 44W steel (
Figure 14c) is primarily driven by HE. As diffused hydrogen accumulates, it weakens the atomic bonds within the steel, particularly along grain boundaries and slip planes, reducing the cohesive strength between atoms. This weakening can facilitate crack initiation either intergranularly along grain boundaries or transgranularly along specific crystallographic planes typical of ferritic steels like 44W [
107,
108,
109]. The fracture process is further influenced by the aforementioned dominant mechanism, HEDE, wherein hydrogen reduces the bond strength between atoms, particularly in high-stress areas like crack tips, thereby promoting brittle failure. Under applied tensile stress, cracks tend to initiate at these hydrogen-weakened regions and propagate in a relatively straight, directional manner, following paths of least resistance. These paths are often perpendicular to the loading direction or specific crystallographic orientations, giving rise to a directional crack morphology. This behavior contrasts with the more random, equiaxed, and dimpled appearance of ductile fractures and is a clear indication of the embrittling effects of hydrogen in 44W steel under tensile loading.
Furthermore, HE causes an increase in the susceptibility of the material to cleavage fracture (
Figure 14b), where cracks propagate along specific crystallographic planes, typically in a brittle manner. The quasi-cleavages (
Figure 14d) seen on the fracture surface result from the material experiencing brittle failure that is not entirely aligned with perfect cleavage planes, but still exhibit characteristics of brittle fracture, often influenced by localized hydrogen-induced weakening [
110,
111]. The formation of microcracks (
Figure 14d) is another consequence of HE. As hydrogen accumulates at grain boundaries, it weakens and embrittles these regions, causing the initiation of microcracks, which propagate transgranularly through the steel, leading to the observed transgranular cracks (
Figure 14b) on the fracture surface.
The fracture surface of Monel 400 charged with 1.30 wppm hydrogen and subjected to uniaxial tensile testing is shown in
Figure 15. As illustrated in
Figure 15a, region 1 (orange) exhibited numerous coalesced voids and a macrocrack, characteristically implying mixed fracture modes in this region but predominantly indicative of ductile fracture behavior. Region 2 (red) showed noticeable elongation of dimples, indicating significant plastic deformation prior to final fracture. Overall, the fracture surface features reflect a combination of predominantly ductile and slightly brittle fracture mechanisms. This behavior is attributed to the limited permeation of hydrogen into the material; while most regions retained the inherent ductility of Monel 400, localized interactions between the infiltrated hydrogen atoms and the microstructure contributed to isolated brittle responses during deformation and failure.
The observed sharp-edge cracks, macrocracks, and cleavage (
Figure 15a,b,d), all characteristic features of brittle failure, are direct results of HE. Macrocracks and sharp-edge cracks primarily form as hydrogen diffuses into the alloy and accumulates in areas of high stress, as previously discussed, leading to the weakening of atomic bonds, followed by crack nucleation and growth under applied tensile stresses. Observed elongated dimples (
Figure 15c) are characteristic of crack initiation and microvoid coalescence, hallmark features of ductile fracture. Their shape and alignment reflect the direction of plastic deformation sustained by the material during tensile loading. While hydrogen can reduce fracture toughness and facilitate cleavage-like fracture along crystallographic planes (
Figure 15d), its limited ingress in this case means these brittle features had a negligible impact on the overall toughness and elongation of the charged Monel 400.
Furthermore, the formation mechanisms of the observed ductile features, elongated dimples, coalesced voids, shear lips, fibrous dimples, and slip regions (
Figure 15a–d), have been thoroughly discussed in earlier sections of this article. However, the wrinkle formations (
Figure 15a), appearing near regions of plastic deformation, such as shear lips or areas adjacent to microvoid coalescence, occurred due to localized plastic instability during deformation. As the material was subjected to tensile stress, slip bands, which are zones of concentrated dislocation movement, formed within the microstructure. These slip bands interact with stress concentrators, such as grain boundaries, inclusions, or other microstructural irregularities, causing uneven deformation and resulting in localized folding or wrinkling on the fracture surface [
112,
113].
Examination of the fracture surface of 1.30 wppm charged 304L austenitic stainless steel (
Figure 16) showed that the material maintained its inherent ductile properties, indicating a negligible to no effect of hydrogen on its mechanical behavior, in agreement with the preceding findings on %elongation and toughness. The fracture surface exhibited macrocracks, microvoids, dimples, shear lips, necking, and tear ridges. The formation mechanisms of the macrocracks, microvoids, dimples, and shear lips (
Figure 16a–d) have been discussed in the preceding sections.
Necking (
Figure 16a) occurs as the material undergoes localized deformation under tensile loading, leading to a reduction in cross-sectional area. This phenomenon is a characteristic of ductile materials, and in this case, the material maintained its ductility despite the hydrogen exposure. Tear ridges (
Figure 16d) are typically observed in ductile fractures formed as a result of localized plastic deformation during fracture, where the material undergoes tearing along specific crystallographic planes [
114,
115]. These ridges develop as cracks propagate through the material, particularly in regions experiencing significant necking. The formation of tear ridges contributes to the roughness and irregularity of the fracture surface, reflecting the material’s resistance to fracture and its ability to undergo substantial plastic deformation before failure.
The fracture surface of the charged arc-DED 308L austenitic stainless steel (
Figure 17) displayed transgranular cracks, secondary cracks, tear ridges, and sharp edges (
Figure 17a–f), all of which resulted from the interaction of diffused hydrogen atoms with its microstructure. Transgranular cracks (
Figure 17d) occur when hydrogen accumulates at both the grain boundaries and within the grains themselves, weakening the atomic bonds and facilitating crack propagation through the grain structure under tensile stress. Consequently, the fracture path follows a transgranular route, with hydrogen promoting brittle failure across the grains.
Secondary cracks (
Figure 17e) form at stress concentrators, such as inclusions, defects, or grain boundaries. Hydrogen intensifies these cracks by damaging the material in localized regions, which advances crack initiation and propagation at points of high stress concentration. As earlier discussed, tear ridges arise from localized plastic deformation as cracks propagate through the material. The presence of hydrogen amplifies the material’s susceptibility to this deformation by lowering the energy required for dislocation motion, leading to an irregular, ridge-like fracture surface.
The EDX analysis of four points (
Figure 17c) on the fracture surface of arc-DED 308L austenitic stainless steel revealed a high weight % of Fe, followed by Cr and Ni (
Table 6). This composition indicates the predominance of the austenite phase, stabilized by the high Ni content, which, together with Cr, enhances the material’s corrosion resistance and ductility.
Additionally, the fracture surface might also contain small regions of ferrite, even though the material is predominantly austenitic. This ferrite could form as a secondary phase due to the rapid cooling during the arc-DED process, which can induce microsegregation of alloying elements. Ferrite, being a BCC phase, can contain a higher iron content, which aligns with the high weight percent of iron detected in the EDX results.
The EDX analysis of the fracture surface of charged arc-DED 308L austenitic stainless steel, as shown in
Figure 17f, reveals intriguing compositional variations across six distinct areas (
Table 7). Five of the analyzed locations, points 1, 2, 4, and regions 5 and 6, exhibited a relatively higher weight % of Fe, followed by Cr. This distribution strongly indicates the expected dominance of the austenite phase in these regions, with the high Fe content further confirming a principally uniform austenitic microstructure, consistent with the typical composition of stainless steels. Cr serves a dual purpose as it stabilizes the matrix while also facilitating the formation of a passive chromium oxide film, essential for the alloy’s remarkable corrosion resistance.
In contrast, point 3 displayed a prominent deviation, with its composition dominated by Mn and Fe. The manganese-rich region observed at point 3 may correspond to inclusions or secondary phases, such as manganese sulfides (MnS) or silicates (Tephroite and Rhodonite) [
116,
117], which occasionally develop in stainless steels during solidification. Tephroite (Mn
2Si0
4) and Rhodonite (MnSiO
4) phases may form under localized conditions where manganese and silicon segregate during rapid solidification. Tephroite, a simple silicate, and Rhodonite, a common inosilicate, are likely to appear in manganese-rich regions with sufficient silicon content, as shown in
Table 7, particularly in areas with high thermal gradients, such as grain boundaries or inclusions [
118]. These inclusions, although not part of the austenitic matrix, can have a significant influence on fracture behavior by acting as stress concentrators or initiating sites for cracks.
The compositional contrast between the Fe- and Cr-rich areas and the Mn-dominated region stresses the essential intricacy introduced by the 3D printing process. While the majority of the material is likely to retain a stable austenitic structure, the presence of localized Mn-enriched phases highlights the potential for microstructural heterogeneity. Such heterogeneity can have critical implications for the mechanical properties and fracture characteristics of the material, pointing out the need for careful consideration of these variations in the context of performance and reliability.