Coupons 1 and 3 were similar in terms of positioning and oxygen access (both were positioned on the bottom of long alumina crucibles with a column of salt on them). However, coupon 1 was part of a long alloy strip, while coupon 3 was a small piece. The shape of oxide scale in coupon 1 is very much defect rich, which makes it less protective in comparison with the compact oxide scale in coupon 3.
As observed in the BSE images in Figs. 2a, d, the oxide scale on coupon 1 was thinner and defect rich. This has led to the base metal being more detectable in the XRD analysis (Fig. 3). Note that the samples were not washed before the XRD analyses to avoid the dissolution of corrosion products. Since more salt had reacted with the alloy surfaces on coupons 2 and 3 which were isothermally exposed, XRD signals of LiF are more pronounced in these samples. The oxide scale in scenario 1 in Fig. 3 exhibits the incorporation of Fe and Cr in addition to Ni. This is in line with the EDX element maps in Fig. 2a, where fluoride has reached underneath the oxide scale and is present deeper in the alloy along grain boundaries in scenario 1. The salt surrounding coupon 1 did not have a yellow color and Li2CrO4 was not detected either in the XRD pattern.
Coupon 2 underwent the most intense fluoride attack of 54 µm deep (Fig. 2b,e). The intergranular attack in this sample is the thickest observed in this study, leading to the detachment of individual grains. This deep intergranular attack is filled with fluoride, which makes the fluoride uptake greater than in scenarios 1 and 3. The oxide scale on this sample is quite heterogeneous, in a way that it rises with very thick nodules up to18 µm thick at some spots, while it is only 5 µm thick at some other spots. This oxide scale in coupon 2 is very much defect rich as can be seen in Fig. 2e, not protective and has not impeded the fluoride ingress during the exposure.
The XRD analysis for coupon 2 (Fig. 3 scenario 2), which was exposed in the horizontal furnace and had continuous access of oxygen, confirms the participation of Cr into the oxide scale. Since Cr has a bigger ionic ratio than Ni, the XRD peaks for Li0.3Cr0.05Ni1.65O in coupon 1 have been slightly shifted to the right in comparison with Li0.4Ni0.6O. The salt surrounding coupon 2, was bright yellow at the salt-alloy interface, which was pointing towards Cr(VI) ions. The XRD pattern in Fig. 3, scenario 2 also confirmed Li2CrO4 as an oxide species, which proves the yellow color observed in the salt.
As shown in Fig. 2c,f, the depth of corrosion attack in coupon 3 (15 µm) has reached only one third of that observed for coupon 1 (54 µm) and the fluoride ingress into the intergranular attack is shallow as well. This is in line with the shape of the oxide scale. A compact, 5 µm thick oxide scale has been formed on coupon 3, which seems to be more protective against fluoride attack. The thickness of the oxide scale is quite similar for coupons 1 and 3 with limited accessibility of oxygen.
The XRD results in Fig. 3 for the oxide scale in scenario 3, which had limited access to oxygen in the vertical furnace, confirms only the participation of Ni. This phenomenon can be attributed to the lack of transport of alloying elements to the oxide scale. Since the fluoride ingress in coupon 3 was not deep into the grain boundaries and only stayed underneath the oxide scale, no increased transport of alloying elements to the oxide scale which is formed of Li0.4Ni0.6O was detected. Since the oxygen activity in the vertical setup was assumed to be low, the oxidation of Cr to Cr(VI) ions was not possible.
After the SEM/EDX analyses, it appears clear that all three scenarios resulted in two distinct reservoirs of fluoride accumulation beneath the metal-oxide interface. The first reservoir accumulates within the Cr, Nb, Fe depletion zone beneath the oxide scale while the second distinct observation of fluoride occurred in the form of decorated grain boundaries reaching deep into the alloy. The extent and depth of this intergranular attack varied between the three scenarios. Scenario 1, which is the sample cut at the hottest part from the long strip, showed the deepest intergranular attack, without causing intragranular depletion within the surrounding grains. In order to investigate more about this sample, the oxide scale after 168 hours was analyzed in Fig. 4 and also exposures on scenario 1 was extended to 1000 hours. The backscattered electron image in Fig. 4 together with the EDX maps for the thermal gradient sample (scenario 1) of alloy Inconel 625 at 600°C shows voids which have been formed underneath the oxide scale. These internal voids are due to the formation of volatile halides (in this case Cr/Fe and Nb fluorides), which provide the means for the metal ions to be transported away from the metal [11]. Fluoride species fill the cavities which are formed underneath the oxide scale. These fluoride pockets are formed within the same layer where chromium and niobium have been depleted and the alloy composition is richer in nickel. It is also evident from the maps that fluoride ingress happens through the grain boundaries and reaches deeper this way. The EDX maps in Fig. 4 show a layered structure for the oxide scale on coupon 1 after 168 hours of exposure. A comparison between EDX maps and the XRD spectra in Fig. 3 for scenario 1 allows for the correlation of oxides scales with lithium constituents. As can be seen in Fig. 4, Cr and Fe are overlapping in some parts in the oxide scale, which leads to the formation of lithiated species of Cr-Fe spinel. The Ni rich (only 5 percent Cr) lithium nickel oxide formed on top of the oxide layers, above the Cr-Fe spinel. Interestingly, an iron and fluoride layer has formed, positioned just in between the nickel rich scale on top and the chromium rich scale beneath. The crystal lattice matching best is an iron-oxy-fluoride species Fe2OF4. As shown in Fig. 3, oxygen did not follow fluoride deeper into the alloy.
These results were compared with the ones from 1000 hours exposure in scenario 1. As can be seen in Fig. 5a, which shows the sample with the temperature gradient (scenario 1) after 1000 hours, the depth of corrosion attack has tripled in comparison with the sample after 168 hours of exposure. Also, the corrosion attack has affected more grains close to the surface. This intergranular attack has become finer below 50 µm. Figure 5b presents the EDX mapping which was done on the top part of the sample to see the behavior of each element after the exposure. It is apparent from the EDX maps that fluoride has reached the deeper grain boundaries, while oxygen has stayed on top. A line EDX scan was done through the first four grains beneath the oxide-metal interface of the sample in order to find out how different elements behave inside the grains and at the grain boundaries. By taking a look at the line scans in Fig. 5c, a depletion zone is noticed beneath the oxide scale for Cr, Fe and Nb. These elements are the same as those which are clearly indicated in the oxide scales shown in Fig. 4. This pattern follows along with fluoride, meaning that when fluoride gets down into the alloy microstructure along the grain boundaries these elements are transported preferentially towards the metal-oxide interface.
As indicated in the line scan in Fig. 5c, depletion profiles for scenario 1 reach as deep as 80 µm into the alloy after 1000 hours. While the intergranular attack by fluorides is progressing significantly deeper, the grains’ interiors are not chemically attenuated after reaching 4 grains beneath the oxide scale. Where the line passes through the smaller grains like grain 1 and 2 in Fig. 5c and where the line scan has been close to the grain boundaries like grain 3, the drop in the counts indicates local depletion. This is while the counts per second for Fe, Nb and Cr have recovered to nominal values in and beyond the fourth grain, where the line scan is located further from the grain boundaries.
It is recognizable in Fig. 5d, that Cr, Nb and Fe are depleted around the grain boundaries where fluoride has access. In this line scan the further we go from the grain boundaries (more pronounced in bigger grains like grain 1 and 4 which are marked both in Fig. 5b and d) Cr, Fe and Nb counts spike, and once the line reaches the grain boundary, the counts per second fall. However, the fluctuation noticed for Mo which are reported in Fig. 5c, shows mostly enrichment in the grain boundaries, where fluoride has reached. This reiterates that fluoride was more passive towards Mo and Ni and did not react to them at the grain boundaries. As a result, it can be said that according to the line scans, Cr, Fe and Nb contributed to the oxide scale which is lithiated. According to the EDX maps, fluoride has formed pockets underneath the oxide scale and permeated deeper into the alloy through the grain boundaries. Considering the line scans in Fig. 5c, it can be inferred that permeating fluoride reacts with Cr, Fe and Nb in grain boundaries and delivers them to the reduced oxygen at the metal oxide interface forming a layered structure oxide scale.