In the present study, thermal stability of α-Ga2O3 under vacuum and ambient pressure conditions was investigated in situ by x-ray diffraction and transmission electron microscopy (TEM). It was observed that the thermal stability of α-Ga2O3 increased by 200 °C when pressure was lowered from an atmospheric to a vacuum level. This finding can be explained by oxygen diffusion under different oxygen partial pressures. In addition, in situ TEM imaging revealed that, once past the decomposition temperature, the onset of phase change propagates from the top crystal surface and accumulates strain, eventually resulting in a fractural film. The mechanism of α-Ga2O3 to β-Ga2O3 transition is evaluated through experiments and is discussed in this manuscript.
I. INTRODUCTION
In the last few years, Ga2O3 has gained tremendous interest for its potential applications in high-power switching and optoelectronics. More specifically, Ga2O3 can be used for detection in smaller wavelengths, such as solar blind deep-UV detectors, due to its ultrawide bandgap (Eg ranging from 4.7 to 5.3 eV).1–7 Ga2O3 can be found in five common polymorph structures: α, β, γ, ɛ (or κ), and δ.8 In particular, β-Ga2O3, which has a monoclinic crystal structure, has been studied extensively as it is the most thermodynamically stable phase.9 Nevertheless, recently, α-Ga2O3 has gained considerable attention for its larger bandgap, at about 5.3 eV.10 α-Ga2O3 also benefits from a corundum-like structure, similar to that of α-Al2O3.11 This similarity in crystal structure suggests that the single crystalline growth of α-Ga2O3 on inexpensive sapphire substrates can be achieved through standard techniques such as mist chemical vapor deposition,10,12,13 pulsed laser deposition,14 and halide vapor phase epitaxy (HVPE).15 Remarkably, Oshima et al. have already succeeded in demonstrating the HVPE growth of high-quality α-Ga2O3 thin films on (0001) sapphire substrates with a high growth rate of 150 μm/h.15
With β-Ga2O3 exhibiting the most stable polymorph, all metastable phases of Ga2O3 eventually transit to the β-phase when exposed to high temperatures. Avoiding this phase change is crucial to maintaining the desired bandgap for a Ga2O3 device and, thus, can be problematic for high-power applications, where temperature fluctuations are inevitable. In order to use the wide bandgap α-phase for such applications, extensive investigation is required to better understand the transition behavior of Ga2O3 under various environmental conditions. One recent study conducted by Cora et al. characterized the dynamics of phase transition for the metastable κ-Ga2O3 under both air and vacuum environments by in situ TEM.16 It was found that for samples subjected to ambient atmospheric pressure, the κ-phase Ga2O3 transitioned to an intermediate γ-phase before ultimately transitioning to the β-phase. However, when under vacuum, κ-Ga2O3 directly transformed into the β-phase structure without the occurrence of any intermediate phase transitions. Additionally, the temperature at which the phase transitions of κ-Ga2O3 occurred was observed to be higher under vacuum levels compared to when exposed to atmospheric pressure.
Specifically, for α-Ga2O3, there are several studies evaluating the stability of α-Ga2O3 at high temperatures for atmospheric pressure conditions. For example, recent studies on α-Ga2O3 in atmospheric pressure demonstrated that the transition from α-Ga2O3 to β-Ga2O3 occurs at temperatures ranging from 600 to 650 °C.17–19 While another study revealed that α-Ga2O3 can remain stable at temperatures as high as 800 °C if a selected-area growth method is used during the heteroepitaxial growth of Ga2O3 on a sapphire substrate.18 However, no research on the study of combined pressure and temperature effects on phase transformation has been conducted thus far. In the present study, the phase transition behavior of α-Ga2O3 under atmospheric pressure and vacuum environments was assessed using in situ x-ray diffraction (XRD) and in situ TEM. And, with these results, a possible mechanism for α to β phase transition is proposed.
II. EXPERIMENT
The two samples used for this study consisted of 4 μm thick α-Ga2O3 films grown on the (0001) sapphire substrate by HVPE under partial pressures p(HCl) = 0.25 kPa and p(O2) = 1.0 kPa at 550 °C. O2 and a mixture of GaCl and GaCl3 were used as precursors, while N2 was used as the carrier gas.20 Further details about the growth process can be found in Refs. 15 and 20.
An in situ XRD study of phase evolution for each α-Ga2O3 film during ramping up the stage temperature was conducted with a Rigaku Smartlab XRD, using a Ge (220) × 2 monochromated Cu source. Two α-Ga2O3 samples were examined in situ by XRD under both ambient and vacuum environments. XRD ω–2θ profiles were recorded at increments of 20 °C starting from 500 °C. Each sample was placed on an Anton Paar DHS1100 Domed Hot Stage with the temperature monitored by a thermocouple. These temperature-dependent measurements were performed both at atmospheric pressure and under vacuum. To achieve vacuum levels, a sample was sealed within the domed hot plate and pumped down to ∼10−4 Torr. For both pressure conditions, the hot plate was first heated at a rate of 20 °C/min until reaching 500 °C. Next, the rate was reduced to 5 °C/min for target temperatures between 500 and 1000 °C. Each target temperature was allowed 5 min to stabilize before recording the XRD profile.
In situ TEM was also performed under similar conditions using a Thermo-Fisher TF30 TEM. The TEM measurements were all conducted under a vacuum environment, at ∼10−7 Torr. A Thermo-Fisher Helios 650 Xe Plasma focused ion beam (FIB) system was used to prepare cross-sectional thin membrane specimens for TEM. The FIB liftouts were then transferred to DENSSolution nanochips and were subsequently mounted onto a DENSSolutions Wildfire double-tilt heating holder. The temperature of the holder was controlled using Impulse software. For the low-pressure environment, a sample was first heated to 400 °C using a ramp rate of 20 °C/min. The rate was then reduced to 5 °C/min for target temperatures higher than 400 °C. TEM bright-field (BF) images and selected-area electron diffraction (SAED) patterns were recorded for each 50 °C interval until the α-Ga2O3 sample visibly transformed into β-Ga2O3. The same TEM experiment at atmospheric pressure was also conducted using the same DENSSolution holder. However, this time the sample was first heated outside of the TEM chamber under an ambient environment from room temperature to 400 °C at the same rate of 20 °C/min. After this initial thermal treatment, the sample was transferred into the TEM chamber for immediate TEM BF and SAED imaging. During the whole process, the sample temperature was maintained by the heating holder. The sample and the heating holder were then taken out of the TEM chamber for heating up to the next target temperature under ambient environment. Similar to the experiments under high vacuum, the sample was observed by TEM for 50 °C increments, starting from 400 °C until α-Ga2O3 fully transitioned to β-Ga2O3 (Fig. 2). This is an example of a figure prepared for double-column publication. Cross-sectional scanning electron microscope (SEM) images of copper zinc tin sulfide films after annealing at (a) and (b) 600 °C, (c)–(e) 700 °C, and (f)–(h) 800 °C for (c) and (f) 30 min, (a), (d), and (g) 1h, and (b), (e), and (h) 2h. All scale bars are 1 μm.
III. RESULTS AND OBSERVATIONS
A. In situ XRD experiments
The α to β phase transitions under both environments were found to occur at 500 and 700 °C, respectively, in our in situ XRD experiments. The XRD ω–2θ profiles are shown in Fig. 1.
As seen in Fig. 1(a), the ω–2θ profiles for atmospheric conditions remained consistent with that of pure α-Ga2O3 for temperatures up to 500 °C. At 500 °C, β-Ga2O3 401 diffraction peak started to occur. A β-Ga2O3 diffraction peak can be observed in ω–2θ scan at 520 °C, indicating the start of the α-Ga2O3 to β-Ga2O3 phase transition. It can also be seen that the α-Ga2O3 0006 peak intensity reduces at these higher temperatures. For the 540 °C profile, additional β-Ga2O3 202 and peaks can also be seen in the XRD profile, with the β-Ga2O3 peak appearing more prominent. For the 560 °C profile, the α-Ga2O3 0006 peak can no longer be seen. Lastly, for temperatures up to 1000 °C, the XRD profile remains the same. After this final temperature had been reached, another ω–2θ profile was performed after the sample had cooled down to room temperature. This XRD profile still exhibits a β-Ga2O3 peak profile, confirming the permanence of the α-Ga2O3 to β-Ga2O3 phase transition.
On the contrary, the XRD ω–2θ profiles measured under vacuum are fixed for temperatures from 20 to 680 °C [Fig. 1(b)]. As seen in the 700 °C profile, the β-Ga2O3 peak is visible and the α-Ga2O3 0006 peak intensity is noticeably reduced. For the 720 °C curve profile, the β-Ga2O3 is also observed and appears to increase in intensity for the 740 °C profile. Once above 720 °C, the α-Ga2O3 peak is no longer visible. Once again, the XRD profile remains unchanged up to 1000 °C. From these data, it can be concluded that the phase transition from α-Ga2O3 to β-Ga2O3 begins at a much higher temperature, around 200 °C higher, for samples under vacuum environments compared to those heated in the atmosphere. The reasons for this increase in the thermal stability of α-Ga2O3, when under vacuum, will be addressed in detail in Sec. IV.
Figure 2 shows SEM images of the α-Ga2O3 sample before and after ramping up the temperature during the in situ XRD heating measurements under the atmosphere. Figure 2(a) presents an as-grown α-Ga2O3 sample, which has a smooth and clear surface. After the sample was heated to 560 °C during the in situ XRD measurements, the sample surface fractured. As discussed earlier, the sample fully transformed into β-Ga2O3 at this temperature [Fig. 2(b)].
B. In situ TEM experiments
Figure 3 shows the TEM results of the experiment performed under atmospheric conditions. Figures 3(a) and 3(b) show the TEM BF image of the as-grown α-Ga2O3 and SAED pattern at room temperature, taken from the sample along its zone axis, respectively. As seen from the TEM BF image, the α-Ga2O3 sample has a high dislocation density. The SAED patterns remained unchanged ramping temperatures up to 600 °C. Once the temperature reached 600 °C, new spots became visible in the SAED pattern, aside from those from α-Ga2O3 [Fig. 3(f)], meaning β-Ga2O3 began to appear. Additionally, dislocations disappeared partially at this temperature. After the temperature was increased to 700 °C, again, more diffraction spots became visible, as seen in Fig. 3(h). The 4 μm membrane specimen fractured when the temperature was raised to 750 °C [Fig. 3(i)]. The SAED pattern taken from this fractured film [Fig. 3(j)] confirmed that the α-Ga2O3 phase fully transformed into β-Ga2O3, which was the same as the SEM observations after XRD experiments.
Figure 4 shows the results of in situ TEM experiments under vacuum. The SAED patterns [Figs. 4(b) and 4(d)] suggest that the α-Ga2O3 phase remained stable up to 700 °C. TEM BF images [Figs. 4(a), 4(c), and 4(e)] also reveal that the dislocation density reduced with increasing temperature. The phase transition began at 800 °C, where points β and β can be seen in the diffraction pattern [Fig. 4(f)]. At 850 °C, the sample fractured [Fig. 4(j)] when it fully transformed into β-Ga2O3, as evident in the SAED [Fig. 4(h)]. The phase transformation under vacuum occurred at a higher temperature than that under ambient temperature. In addition, the phase transformation from α-Ga2O3 and β-Ga2O3 during the TEM measurement happened at a higher temperature than that during the XRD measurement. These results will be discussed in detail in Sec. IV.
Figure 5 shows the in situ TEM diffraction patterns for different locations of the sample heated to 600 °C under atmospheric pressure. From these images, it can be concluded that the phase change began at the surface of the sample. Figure 5(a) shows that the zone axis of [001]β occurred on the top surface, while the other areas of the sample consisted of only α direction [Figs. 5(b)–5(c),]. Any other spots in the pattern besides α in Fig. 5(c) could be attributed to the zone axis of the sapphire substrate. Figures 5(e) and 5(f) show the crystal structures of α-Ga2O3 and β-Ga2O3 aligned along the α and [001]β directions, respectively.
Table I summarizes the experiments results of both TEM and XRD experiments in ambient and vacuum environments conducted at different temperatures.
Sample No. . | Experimental environment . | Analysis method . | Ramp rate . | Scanning temperature . | Phase transition temperature (°C) . |
---|---|---|---|---|---|
1 | Vacuum | XRD analysis | T ≤ 500 °C: 20 °C/min | Every 20 °C when T > 500 °C | 680–700 |
2 | Ambient | 500–520 | |||
T > 500 °C: 5 °C/min | |||||
3 | Vacuum | TEM analysis | T ≤ 400 °C: 20 °C/min | Every 50 °C when T > 400 °C | 800 |
4 | Ambient | T > 400 °C: 5 °C/min | 600 |
Sample No. . | Experimental environment . | Analysis method . | Ramp rate . | Scanning temperature . | Phase transition temperature (°C) . |
---|---|---|---|---|---|
1 | Vacuum | XRD analysis | T ≤ 500 °C: 20 °C/min | Every 20 °C when T > 500 °C | 680–700 |
2 | Ambient | 500–520 | |||
T > 500 °C: 5 °C/min | |||||
3 | Vacuum | TEM analysis | T ≤ 400 °C: 20 °C/min | Every 50 °C when T > 400 °C | 800 |
4 | Ambient | T > 400 °C: 5 °C/min | 600 |
IV. DISCUSSIONS
From the experiments above, we can conclude that α-Ga2O3 to β-Ga2O3 phase transition: (i) completes at dozens of degrees higher than the phase transition starts; (ii) starts at the surface of materials and results in fracturing the film; (iii) occurs at 100 °C lower by XRD measurements than that by TEM measurements under similar conditions; and (iv) occurs at ∼200 °C higher under vacuum than that under ambient environment. It is reported that the phase transition temperature for α-Ga2O3 to β-Ga2O3 under atmospheric pressure is between 600 and 650 °C.17–19 α-Ga2O3 to β-Ga2O3 phase transition can be characterized as a pseudomartensitic transformation, which mainly involves two steps: (a) the repeated O sublattice transformation by shearing close-packed O layers and (b) the periodical reordering of Ga.21,22 Pseudomartensitic transformation is a multistep and multitype phase transition. In our case, several structurally ordered sublattices GaOx, (x = 4, 5, and 6) are involved during the transition. One feature of such transformation is that the phase transition is a slow process because of multitype reactions and the high energy barrier of atom reconstruction (1). This feature is observed in our experiments: after the first β occurrence, the α to β phase transition was not completed until the samples were heated for more than 30 min and at higher temperatures. Jinno et al. hypothesize that the thermal stress in α-Ga2O3 mainly contributes to the α to β phase transition.13 They have pointed out that samples will bend under high temperatures due to the differences in the thermal expansion coefficients of sapphire and α-Ga2O3 layer.17,23,24 When bending, strain is induced and accumulated at the surface of the sample and stress is accumulated at the bottom of it. When approaching a critical temperature, the strain at the top of the thin film accumulates to an extent that can lead to a slip plane shift, which results in the start of α to β phase transition.25 Moreover, it is also known that the α-Ga2O3 layer has in-plane compressive stress at the interface of the sapphire substrate due to the lattice mismatch.12 Such compressive stress can partially compensate for the thermal stress and results in the bottom layer being more unlikely to start the phase transition than the top layer. It is also observed that the phase transition temperature is ∼100 °C lower in XRD studies than in TEM studies in the same environment. This is because of the different sizes of the samples that were used for each experiment. Jinno et al. also reported that selective-area grown α-Ga2O3 could enhance thermal stability due to reducing dislocation density and thermal stress in the window patterns (15). In our XRD experiments, a 2-in. α-Ga2O3 wafer was diced into 10 × 10 mm2 square samples for the XRD measurements, whereas the TEM specimens were ∼6 μm wide, ∼120 nm thick, and several micrometer long. During thermal treatments, thermal strain can be more released in the nanoscale specimen (those used for TEM studies) than the larger samples (those used for XRD studies), which results in the α to β phase transition starting at a lower temperature than the TEM study specimen.
The higher thermal stability of α-Ga2O3 under a vacuum environment may be due to the differences in O2 partial pressure (pO2). As mentioned above, O sublattice transformation and Ga reconstruction are the two elementary steps of α to β phase transition. The higher coordination number of Ga–O intermediates such as (GaOx, x = 4, 5, and 6) are formed during the phase transition.21 The concentration of these high number O coordinated intermediates decreases under a low pO2 environment, which limits the O diffusion in Ga2O3 and increases the overall energy barrier of the phase transition.26,27 Compared to atmospheric environment (pO2 = 0.21 atm), pO2 is nearly zero under vacuum environment. As a result, the α to β phase transition is more difficult under a vacuum environment, leading to a higher thermal stability of α-Ga2O3.
V. SUMMARY AND CONCLUSIONS
Both in situ XRD and in situ TEM experiments revealed that the α-Ga2O3 to β-Ga2O3 phase transition temperature increased by 200 °C under a high vacuum environment than under ambient conditions. This observation is explained by the impact of oxygen partial pressure on oxygen diffusion. The XRD results indicated that the large α-Ga2O3 piece started to transform into β-Ga2O3 at 500 and 700 °C under ambient and vacuum, respectively. The phase transition under both environments was completed at dozens of degree Celsius higher than the first occurrence of the β phase. Fractured films were observed under both SEM and TEM images after the α to β phase transition completed. The in situ TEM observations showed that the phase transition temperature for nanoscale α-Ga2O3 sample was 600 °C under ambient environments and 800 °C under high vacuum. In addition, TEM observations also revealed that with the increase in temperature, the dislocation density of α-Ga2O3 sample decreased and the α to β phase transition started at the top surface. The result of the phase transition temperature is ∼100 °C higher under TEM experiments than the temperature under XRD experiments, which can be explained by the difference in strain accumulation under different sizes of samples.
ACKNOWLEDGMENTS
This work was supported by the Air Force Office of Scientific Research (Program Manager, Dr. Ali Sayir) through Program FA9550-20-1-0045 and the National Science Foundation (NSF) under Grant No. 2043803. The authors also acknowledge the financial support of the University of Michigan College of Engineering for the Thermo-Fisher G4 650 Xe Plasma-FIB and TF30 in situ ion irradiation TEM.
AUTHOR DECLARATIONS
Conflict of Interest
The authors have no conflicts to disclose.
Author Contributions
Zhuoqun Wen: Conceptualization (equal); Data curation (equal); Formal analysis (equal); Investigation (equal); Methodology (equal); Writing – original draft (equal). Kamruzzaman Khan: Conceptualization (equal); Formal analysis (equal); Investigation (equal); Methodology (equal); Writing – review & editing (equal). Kai Sun: Data curation (equal); Formal analysis (equal); Investigation (equal); Methodology (equal). Ruby Wellen: Data curation (equal); Formal analysis (equal); Writing – original draft (equal). Yuichi Oshima: Data curation (equal); Formal analysis (equal); Investigation (equal); Methodology (equal); Writing – review & editing (equal). Elaheh Ahmadi: Data curation (equal); Formal analysis (equal); Funding acquisition (lead); Methodology (equal); Resources (lead); Writing – review & editing (equal).
DATA AVAILABILITY
The data that support the findings of this study are available from the corresponding author upon reasonable request.