2.1. HR SR-PXD and PND
The structural properties of the intermetallic powders were investigated using both HR SR-PXD and PND techniques to obtain sufficient contrast among the system elements, while SR-PXD data helped to differentiate between La and Y, the PND measurements allowed to distinguish the Mn and Ni atoms. The combined simultaneous analysis of both data sets, carried out for each composition, appears essential for the accurate analysis of the material crystal structures (
Figure 1,
Figure 2 and
Figure 3 and
Table 1,
Table 2,
Table 3 and
Table 4). The results confirm the formation of
H-A
2B
7 as a main phase in all studied samples. The higher Y content results in the shifting of Bragg peak positions towards higher 2
angles in the collected diffraction patterns, which indicates the formation of a smaller unit cell, as expected (atomic radius of La = 1.87 Å and Y = 1.79 [
39]) and previously reported [
34,
35]. The substitution of Ni by Al or Mn atoms (atomic radius of Ni = 1.26 Å, Al = 1.41 Å, Mn = 1.32 Å [
39]), were expected to influence the average unit cell size, as also reported by other studies [
30,
38].
The Rietveld refinement results indicate the formation of a single hexagonal Ce
2Ni
7-type phase only in Y
0.67 and Y
1.00. In all other samples, additional secondary phases are present (
Table 1). Y
0.33 consists of
H-A
2B
7 (95 wt.%) and the minor AB
5-type (5.3 wt.%) phase. The concentration of the major
H-A
2B
7 increases to 100 wt.% in Y
0.67 and Y
1.00 but again decreases to 89 wt.% and 53 wt.% for Y
1.33 and Y
1.67, respectively. In the samples with the higher Y concentration (x ≥ 1.33), the formation of the
R-A
2B
7 and
R-AB
3 phases has also been observed, which confirms but also contradicts some of the previously reported results. Liu et al. [
34] (La
3-xY
xNi
9.7Mn
0.5Al
0.3 (x = 1, 1.5, 1.75, 2, 2.25, 2.5)) claimed that the increased Y concentration stabilised the formation of
H-A
2B
7, whereas Zhao et al. [
35] (La
1-xY
xNi
3.25Mn
0.150Al
0.10 (x = 0.00–1.00)) observed the presence of the
H-A
2B
7 phase only up to x ≥ 0.85, and the
R-AB
3 phase occurrence for higher Y content. The findings presented herein confirm that the Y presence induces the formation
H-A
2B
7 in the entire sample series, but the higher Y concentration (x ≥ 1.33) leads additionally to crystallisation of the
R-A
2B
7 and
R-AB
3 phases. Our observations are in line with earlier reports, suggesting that A
2B
7 compositions with a higher concentration of smaller A elements, e.g., Y, prefer to take rhombohedral symmetry instead of hexagonal one [
40,
41], which is in line with the higher abundance of the
R-A
2B
7 phase in Y
1.33 and Y
1.67.
The refined lattice parameters of the major
H-A
2B
7 phase decrease with the increasing Y content (
a =
b = 5.0740 and 5.0004 Å for Y
0.33 and Y
1.67, respectively;
c = 24.643 and 24.322 Å for Y
0.33 and Y
1.67, respectively), resulting in smaller subunit (
V
A2B4 = 6.4% and
V
AB5 = 2.9%) and unit cell volumes (
V = 4.2%) as seen in
Table 1. (The subunit volumes are calculated using
where
is the unit cell volume,
c is the lattice parameter, and
and
are z value coordinates between 0 and 1 of the atoms at the edge of the subunit).
To help determine the quality of the fitted parameters, the
Rwp and
RBragg are shown in
Table 2 and
Table 3, respectively. As seen for
Rwp, the values might seem high. Still, one must remember that when dealing with higher quality datasets, these may, in turn, provide higher
Rwp values due to imperfections not considered in the data refining step. On the other hand, the
RBragg values are generally small, indicating that the chosen model is satisfactory.
As shown in
Table 4, the Y occupancy factor at the
4f1 and
4f2 sites in
H-A
2B
7 increases from 0.14 to 0.70, and from 0.09 to 0.26 for Y
0.33 and Y
1.00, respectively. With the higher Y content, the element concentration at the
4f1 and
4f2 sites rise further to reach eventually 93 and 84%, respectively, in Y
1.67. This suggests that while initially, Y occupy the A
2B
4 subunits, once filled up (x ≥ 1), it prefers entering the AB
5 subunits. Such behaviour has been previously reported and was related to a lower coordination number of 16 at the
4f1 site when compared with coordination number 20 at the
4f2 site [
36]. The higher Y concentration in the samples also shortens the
4f1-
4f1 distance in the neighbouring unit cells from 3.282(3) to 3.170(7) Å for Y
0.33 and Y
1.67, respectively.
The Rietveld refinement results indicate that Mn atoms are present at the
4e and
6h sites in all studied compositions. The obtained fractional occupancies are low but larger than the estimated standard deviation values. In Y
0.33, Y
0.67 and Y
1.00, Mn appears additionally at the
4f3 site. This site depletion observed in the Y-rich compositions, correlates with a subtle increase of the Mn atom occupancies at
4e and
6h, similar to the result reported by Deng et al. [
31] for Y
0.75La
0.25Ni
3.2Mn
0.3 with
H-A
2B
7 crystal structure.
In Y
0.33, Y
0.67 and Y
1.00, the Al atoms are distributed over the
6h and
12k sites, with the latter being less occupied. This is in line with the earlier report by Wang et al. [
38]. They found that for
H-A
2B
7 in the LaY
1.9Ni
10.2-xAl
xMn
0.5 (x = 0, 0.2, 0.4, 0.6) system the presence of Al was only detected at the
6h site, between two AB
5 subunits. Similar results were also observed for
H-A
2B
7 formed in La
0.77Mg
0.23Ni
3.41Al
0.09 and Nd
0.9Mg
0.1Ni
3.3Al
0.2 [
21,
42]. In Y
1.33 and Y
1.67, the
6h site is no longer populated by Al, but at the same time, a slight increase of aluminium concentration at the
12k site is observed. These findings, compared with the changes in population of the
4f1 and
4f2 sites, may indicate that the higher amount of Y atoms in
H-A
2B
7, and its increasing concentration at the
4f2 site, have an effect on (correlates with) the B atom distribution over the available crystallographic sites in this crystal structure, however the nature of interatomic relationships must be further investigated.
2.4. PCT
The PCT measurements (
Figure 6) were performed for Y
1.00, Y
1.33 and Y
1.67 to investigate in detail, the material hydrogen absorption behaviours. The corresponding Van’t Hoff plots are shown in
Figure 6d. The values of the enthalpy and entropy of the hydride formation in the studied samples, along with the expected plateau pressures at 30 °C, are listed in
Table 7.
No leaks were detected during the pre-hydrogen exposure setup. For each point of the PCT a step time of 1.5 h has been chosen in order to obtain a PCT measurement with satisfactory accuracy. As an example,
Figure S5 of the supplementary information shows a representative kinetics curve obtained for one point during the PCT measurements.
As highlighted in the paper by Rudman [
45], great care needs to be taken when measuring the PCT characteristics of a material. A very high
P (40 bars) was chosen during activation, and hydrogen was completely absorbed within minutes. During the PCT measurements, a
P of 2 bars was set for each point, with the sample experiencing a
P of approximately 1 bar due to the reservoir and sample holder volumes described in the experimental section. Here, most hydrogen had been absorbed within minutes, with the absorption being greatly slowed down after 30 min of hydrogen exposure.
While the PCT plot for Y
1.00 (
Figure 6a) revealed only one clearly visible plateau pressure, at all studied temperatures, the data for Y
1.33 and Y
1.67 (
Figure 6b,c) displayed two hydrogen absorption regions. Furthermore, the single plateau of Y
1.00 occurs at a higher hydrogen pressure value (2.9 bar of H
2 at 50 °C) than any of the highest plateaus observed for Y
1.33 and Y
1.67 (0.6 and 1.6 bar of H
2 at 50 °C for Y
1.33 and Y
1.67, respectively). Previous studies showed that for La
2Ni
7-based materials, either single [
46] or multiple [
37] plateau pressures can be expected for both single phase (
H-A
2B
7 or
R-A
2B
7) or combined phase materials. It has been discussed that if more than one plateaus were present, it was likely due to: (a) the existence of multiple hydrogen-active (absorbing) phases in the sample [
47], and/or (b) the hydrogen absorption at different pressures by various structural subunits [
37]. The PCT data presented in
Figure 6 differ from those reported in literature for similar compositions, both in the number of plateaus and, in the case of Y
1.00, the equilibrium pressures [
34,
35,
37]. Single plateaus in A
2B
7-type compounds can be obtained by adjusting the subunit volumes [
37].
As mentioned earlier, there can be two potential reasons for the appearance of the two plateaus as observed in Y
1.33: The appearance of multiple phases [
47], or subunits absorbing at different pressures [
37]. Since both samples contained multiple phases, it could be assumed that this was the reason for the multiple plateaus. However, for La
2-xY
xNi
7 Zhang et al. [
37] argued that the appearance of the multiple plateaus were not due to the
H-A
2B
7 or
R-A
2B
7 phases appearing at the same time, but rather the different subunits absorbing at different pressures due to a difference in volume size.
For Y
1.67 (
Table 1), a
R-AB
3 phase was present in addition to the
H-A
2B
7 and
R-A
2B
7-type phases. Earlier studies have found that the equilibrium pressures of
R-AB
3 were expected to be similar to that of
H-A
2B
7 due to the similarities in their superstacking structures [
48,
49]. As such, it was considered that the appearance of two plateaus in Y
1.33 and Y
1.67 was not due to the appearance of different phases, but due to differences in the subunit volumes in these phases.
By increasing the ratio Y/La our measurements showed a higher gas storage capacity (1.37 wt.% for Y
1.00 vs. 1.60 wt.% for Y
1.67, both at 50 C (
Table 8)). This was partly attributed to the lower weight of Y compared to La, though the large increase in capacity from Y
1.00 (1.37 wt.% at 50 °C) to Y
1.33 (1.57 wt.% at 50 °C) cannot be explained by the sole relative weight difference between La and Y.
When performing PCT at various temperatures, for each sample a loss of storage capacity was observed as the temperature increase (
Figure 6 and
Table 8), with a more marked change from 70 °C to 90 °C (between 0.05 and 0.10 wt.% difference) than from 50 °C to 70 °C (between 0.02 and 0.05 wt.% difference). Furthermore, the major changes were observed in Y
1.00, compared to the changes for Y
1.33 and Y
1.67.
According to various findings, the plateau pressure values are affected by either a local chemical (binding) environment between the hydrogen atoms and the metallic atoms in the crystal structure (both A and B elements) [
50], and/or differences in unit cell size [
51]. According to Khatamian and Manchester [
52], the formation enthalpy of YH
2 is −219.6 kJ/mol(H
2) close to other findings [
53], whereas that of LaH
2 is −208 kJ/mol(H
2) [
50,
54]. This difference indicates that a higher La-content in the sample should result in higher plateau pressure values. In our case, as indicated by the values obtained for Y
1.33 and Y
1.67 (
Figure 6b,c) it was observed that with increasing Y content the plateaus increased. It is important to note that the plateau pressure were higher for Y
1.00 (
Figure 6a), when compared to Y
1.33 and Y
1.67. This goes against the expected trend, seeing as others have shown for A
2B
7-type materials based on La-Y-Ni the plateau increased the more Y was present, due to a decrease in the average unit cell size [
34,
35,
37]. Further, Zhang et al. [
37] showed that in case the two plateaus were due to absorption in the different subunits, the lower plateau pressure can be related to the volume of the A
2B
4 subunit, in that if the subunit volume decrease, the lower plateau pressure increase. The higher plateau was more complex and requires a more thorough inspection, since some substitutions lead to plateau pressure stabilization, even with changes to the subunit volumes [
37].
The measured hydrogenation pressures for Y
1.00 absorbed from 2.9 bar at 50 °C to 9.3 bar at 90 °C, for Y
1.33 the lower plateau pressure absorb from 0.2 bar at 50 °C to 0.8 bar at 90 °C, the higher pressure go from 0.6 bar at 50 °C to 2.2 bar at 90 °C. Y
1.67 displayed a lower plateau absorbing from 0.4 bar at 50 °C to 1.6 bar at 90 °C and a higher plateau of 1.6 bar at 50 °C to 5.7 bar at 90 °C. From these measurements the enthalpy and entropy of formation, using a Van’t Hoff plot as shown in
Figure 6d. From these, the pressure plateaus at 30 °C were calculated (
Table 7).
Liu et al. [
34] found that for La
3-xY
xNi
9.7Mn
0.5Al
0.3 (x = 1, 1.5, 1.75, 2, 2.25, 2.5) all samples had two plateaus (found via electrochemical measurements). For a composition similar to Y
1.00 (La
1.5Y
1.5Ni
9.7Mn
0.5Al
0.3) the plateaus were at roughly 0.02 bar and 0.07 bar, for La
1.0Y
2.0Ni
9.7Mn
0.5Al
0.3 (similar to Y
1.33) the plateaus were at 0.06 bar and 0.2 bar. Lastly for La
0.5Y
2.5Ni
9.7Mn
0.5Al
0.3 (similar to Y
1.67) the plateaus were at 0.07 bar and 0.3 bar.
Zhao et al. [
35] found that La
1-xY
xNi
3.25Mn
0.15Al
0.10 (x = 0.00–1.00) showed both single and multiple plateau behaviour. When looking at the compositions La
0.5Y
0.5Ni
3.25Mn
0.15Al
0.10, La
0.33Y
0.67Ni
3.25Mn
0.15Al
0.10 and La
0.12Y
0.85Ni
3.25Mn
0.15Al
0.10 (comparable to Y
1.00, Y
1.33 and Y
1.67, respectively) only single plateaus were observed at 0.26 bar, 0.54 bar and 0.94 bar, respectively.
When comparing all of these literature plateau pressure values with the plateau pressures calculated at 30 °C, it was observed that for Y
1.00 the calculated plateau was higher than reported values in the literature for both single and multiple plateaus. When comparing the calculated plateau pressures of Y
1.33 and Y
1.67 to the plateau pressures found by Liu et al. [
34] it was observed that all calculated plateau pressures reported here were higher, than the electrochemically measured plateaus reported by Liu et al. By comparing the calculated plateau pressures to those obtained by Zhao et al. [
35], it was observed that the single plateaus reported by Zhao et al. have higher plateau pressures, than both of the calculated plateau pressures.
As described, there are no clear trends in the literature regarding this compound, both regarding plateau pressures, but also the number of plateaus. The reported data correspond to this in that no clear trends were found, showing that the picture is more complex, and great care needs to be applied to all known aspects that can affect the hydrogenation properties.
Figure 7 shows the PXD data collected for the three samples before and after PCT experiments, with sample completely desorbed (here called after exposure). The sample with the lowest yttrium concentration (Y
1.00) become less crystalline after exposure to hydrogen gas as compared to Y-rich compositions. This suggests that higher Y content helps to retain material crystallinity during hydrogen ab/desorption.
Fang et al. [
55] found that if the volumes of the A
2B
4 and AB
5 subunits in a variety of AB
3-type intermetallics (PrNi
3, NdNi
3, SmNi
2.67Mn
0.33, SmNi
3, Sm
0.9Mg
0.1Ni
3 and Nd
0.33Er
0.67Ni
3) were smaller than 89.2 Å
3 and 88.3 Å
3, respectively, then the material could release all of the absorbed hydrogen. When above these limits, the hydrogen could not be completely desorbed from their respective subunits. The critical volume limits were further confirmed by Zhang et al. [
37], who studied a variety of La
xA
2-xNi
7, (A = Gd, Sm, Y, Mg). Samples of La
xY
2-xNi
7 with x between 0 and 0.8, had subunit volumes below these critical values mentioned above, and showed the best cycling behaviour.
Among the three hydrogenated samples presented here, only the A
2B
4 and AB
5 subunits of the Y
1.67 intermetallic were below the critical values of 89.2 Å
3 and 88.3 Å
3 (
Table 1). When analysing the XRD data before and after hydrogenation, Y
1.67 was also the sample with the best-preserved crystallinity after sample activation and three PCT hydrogenation cycles (
Figure 7). Thus, the loss in crystallinity and lower capacity for samples with lower Y content may be due to partial hydrogen release. For Y
1.00 and Y
1.33, while the volumes of the A
2B
4 subunits exceeded the critical values, sizes of the AB
5 subunits were rather borderline values, with Y
1.33 being just above the limit. This may explain the appearance of the secondary plateau in the case of Y
1.33, as well as the better crystallinity and hydrogen release compared to Y
1.00. In the case of Y
1.67 the volume values were below the critical limit for both subunits and confirmed the link with better crystallinity compared to the other samples, and the most well-defined plateau regions. Further investigations are needed to confirm this hypothesis.