The delivery of an elemental cation flux to the substrate surface in the oxide molecular beam epitaxy (MBE) chamber has been utilized not only for the epitaxial growth of oxide thin films in the presence of oxygen but also in the absence of oxygen for the growth temperature calibration (by determining the adsorption temperature of the elements) and in situ etching of oxide layers (e.g., Ga2O3 etched by Ga). These elemental fluxes may, however, leave unwanted cation adsorbates or droplets on the surface, which traditionally require removal by in situ superheating or ex situ wet-chemical etching with potentially surface-degrading effects. This study demonstrates a universal in situ approach to remove the residual cation elements from the surface via conversion into a volatile suboxide by a molecular O2-flux in an MBE system followed by suboxide evaporation at temperatures significantly below the elemental evaporation temperature. We experimentally investigate the in situ etching of Ga and Ge cation layers and their etching efficiency using in situ line-of-sight quadrupole mass spectrometry and reflection high-energy electron diffraction. The application of this process is demonstrated by the in situ removal of residual Ga droplets from a SiO2 mask after structuring a Ga2O3 layer by in situ Ga-etching. We predict this approach to be generally applicable in MBE and metalorganic chemical vapor deposition to remove residual elements with vapor pressure lower than that of their volatile suboxides or oxides, such as B, In, La, Si, Sn, Sb, Mo, Nb, Ru, Ta, V, and W.
I. INTRODUCTION
Transparent semiconducting oxides like Ga2O3, In2O3, SnO2, and GeO2 have been rediscovered as promising (ultra-)wide bandgap semiconductors for applications in power electronics.1–5 Their growth as epitaxial thin films by molecular beam epitaxy (MBE) is beneficial for materials exploration and device applications, both requiring a high-degree of purity and crystallinity.
In the MBE growth of oxides possessing volatile suboxide such as Ga2O3, In2O3, SnO2, and GeO2 from elemental sources (Ga, In, Sn, and Ge), the provided elemental flux is oxidized via a first oxidization step to form suboxides (Ga2O, In2O, SnO, and GeO) on the substrate. The suboxide is further oxidized via a second oxidization step to form solid oxide thin films.6,7 The competing desorption of the intermediately formed suboxide (typically having a higher vapor pressure than its cation element) can decrease the thin film growth rate. While in an oxide MBE-growth chamber, suboxides were also found to form (and evaporate) readily from the elemental sources at a typical molecular O2 background pressure present during growth,8,9 their oxidation into the stable oxide (e.g., Ga2O3, In2O3, SnO2, GeO2, and SiO2) required more reactive oxygen species, e.g., provided by an oxygen plasma.7,8,10–13 Solely, the growth of In2O3 at a low growth rate of 0.6 nm/min has been demonstrated using molecular O2.14
Despite these beneficial applications, the elemental fluxes are prone to leave unwanted elemental adsorbates, layers, or droplets on the surface. The removal of these elemental layers requires heating to the desorption temperature of the element, high-energy sputtering, or ex situ wet-chemical etching—all of which may create unacceptable degradation of the surface.
II. EXPERIMENT
A. Deposition of Ga and Ge layers
For this study, Ge and Ga cation layers were grown in high vacuum (background pressure 10−8 mbar) on 2-in. c-plane sapphire [Al2O3(0001)] wafers at a temperature of 400 °C by MBE. The rough backside of the single-side polished substrate was sputter-coated with titanium to allow for noncontact substrate heating by radiation from the substrate heater. The substrate temperature (Tsub) was measured with a thermocouple placed behind the substrate heater. Standard shuttered effusion cells were used to evaporate Ge (7 N purity) and Ga (7 N purity) from pyrolytic BN crucibles. The beam equivalent pressure (BEP) of the cations and O2, proportional to the particle flux, were measured by a nude filament ion gauge positioned at the substrate location. A schematically drawn MBE growth chamber used in this study can be seen in Fig. 2. Table I illustrates the geometries of all the used MBE components. The BEPs are given in units of mbar and are converted into the equivalent particle flux (atoms cm−2 s−1) by multiplying the measured growth rate of the GeO2 and Ga2O3 layer under conditions of full Ge and Ga incorporation by the cation number density of rutile phase GeO2 (2.4 × 1022 cm−3)7 and monoclinic phase Ga2O3 (3.6 × 1022 cm−3)28 and by kinetic gas theory in the case of O2. For layer deposition, the used Ge and Ga -cell temperatures of 1300 °C (Note that this high temperature leads to a relatively fast degradation of the used standard effusion cell.) and 900 °C resulted in Ge and Ga-fluxes (Φ) of ΦGe = 2.2 × 1014 cm−2 s−1 and ΦGa = 2.2 × 1014 cm−2 s−1 impinging on the substrate, respectively.
. | Polar coordinate of normals . | Distance to substrate . | |
---|---|---|---|
MBE setup . | Θ (o) . | Ψ (o) . | L (cm) . |
Substrate | 180 | 0 | 0 |
QMS | 21 | 116 | 15 |
Ge cell | 21 | 64 | 15 |
Ga cell | 40 | 132 | 15 |
O2 source | 33 | 180 | 15 |
. | Polar coordinate of normals . | Distance to substrate . | |
---|---|---|---|
MBE setup . | Θ (o) . | Ψ (o) . | L (cm) . |
Substrate | 180 | 0 | 0 |
QMS | 21 | 116 | 15 |
Ge cell | 21 | 64 | 15 |
Ga cell | 40 | 132 | 15 |
O2 source | 33 | 180 | 15 |
B. In situ removal of the deposited cation droplets or layers
Next, we provided molecular O2 to etch the deposited Ga and Ge layers at elevated substrate temperatures (650 °C for Ga and 700 °C for Ge) that allow suboxides to desorb. For this purpose, a mass flow controller supplied molecular O2 from the research-grade O2 gas (6 N purity) and the O2 flow was set as standard cubic centimeters per minute (SCCM). The flux Φ of desorbing species from the layer surface was measured in situ by line-of-sight quadrupole mass spectrometry (QMS, Hiden Analytical “HAL 511 3F”). The QMS ionizer was run at an electron energy of 50 eV to obtain optimal sensitivity. Therefore, some of the measured signals might be affected by fragmentation of suboxide molecules into cation and oxygen atoms.29 To assess the surface coverage, the process was additionally in situ monitored by reflection high-energy electron diffraction (RHEED). The electron gun supplies electrons with kinetic energy of Ekin = 20 keV impinging on the growth surface at grazing incidence <2o. Scattered electrons are hitting a phosphor screen positioned in the diffracted beam path and the resulting image is recorded by a CCD camera.
As an application example, we demonstrate the in situ removal of Ga droplets from a SiO2 mask directly after in situ patterning of Ga2O3 by Ga-etching. For this purpose, an MBE-grown, ≈500 nm-thick Ga2O3 layer was covered by a ≈75 nm-thick SiO2 hard mask (deposited using sputtering and structured by contact lithography and CHF3-based reactive ion etching) and subsequently loaded into the MBE growth chamber. Ga-etching was performed by exposure to a Ga flux of ΦGa = 6.6 × 1014 cm−2 s−1 at Tsub = 650°C in the absence of O2 for a total etching time of 40 min, resulting in an etch depth of ≈140 nm (determined by profilometry measurement). Subsequently, we in situ removed the Ga droplets that remained on the SiO2 mask by exposure to 1 SCCM O2 for 90 min at the same Tsub. The untouched structured-Ga2O3 sample, the structured-Ga2O3 sample after Ga-etching, as well as a Ga-etched Ga2O3 sample after molecular O2 exposure were observed by top-view scanning electron microscopy (SEM).
III. RESULTS AND DISCUSSION
A. In situ etching of Ga layers
Figure 3 presents the QMS signal of Ga and Ga2O (proportional to the desorbing flux of ΦGa and and the corresponding RHEED images at different stages during the elemental layer deposition and its subsequent etching by O2. When the Ga shutter was opened, the elemental desorption slightly increased and then rapidly faded, corresponding to an almost full adsorption of the provided flux. After closing the Ga shutter, Tsub was immediately increased to 650 °C at 0.5 °C/s to facilitate Ga2O desorption in the following etching process. The elevated Tsub did not result in detectable desorption of the already grown cation layer (the QMS signal before supplying O2 is negligible), while the disappeared streaky RHEED pattern (middle) clearly indicates a substrate coverage by this layer. A dramatic signal increase can be observed when an O2 flow (1 SCCM) started impinging on the surface. This observation confirms that O2 reacted with Ga to form Ga2O via Eq. (3) at a temperature that allows suboxides to desorb. fades gradually from the maximum value, likely due to the gradual decrease of surface fraction covered by the elemental layer. The Ga signal during etching is related to the fragmentation of Ga2O molecules by the electrons of the ionizer in the quadrupole mass spectrometer.29 The complete removal of the Ga layer is evidenced by the disappearance of the signal and by the reappearance of the streaky RHEED pattern of the substrate.
B. Etching efficiency of O2 to Ga layers
To determine the efficiency of the etching process, we established a quantitative relation of impinging O2-flux and desorbing Ga2O flux at varying flow rates of O2. Figure 4(a) illustrates the QMS signal of during the deposition of 6 equal layers of metallic Ga and their in situ etching by O2 at a decreasing flow, which were 2.00, 1.50, 1.00, 0.80, 0.50, 0.25 SCCM, respectively. These experiments were carried out in sequence using Ga deposition and etching temperatures of 400 and 650 °C, respectively. Similar to Fig. 3, a sharp increase of was detected when O2 was supplied, and different O2-fluxes were able to fully convert the Ga layers into evaporated Ga2O, leaving behind a clean surface. Apparently, the maximum decreases with reduced impinging O2-flux and the required time to completely remove the same amount of Ga increases simultaneously.
C. In situ etching of Ge layers
The QMS signal of the desorbing ΦGe and ΦGeO, as well as the surface development monitored by RHEED during Ge layer deposition and O2-etching experiment, shown in Fig. 6, exhibit qualitatively similar behavior to that observed for Ga. To enhance GeO desorption in the etching process, O2 was supplied at Tsub = 700 °C. A significant ΦGeO signal increase can be observed when the O2 (1 SCCM) approached the surface, confirming that O2 reacted with Ge to form GeO via Eq. (4). The disappearance of ΦGeO and reappearance of the streaky RHEED pattern of the substrate proved a complete removal of the Ge layer. Similarly, we determined η for Ge etching using the same methodology employed in our Ga experiment. A surface coverage of DGe = 7.85 × 1017 cm−2, a desorbing flux of ΦGeO = 1.58 × 1014 cm−2 s−1 was obtained based on the using experiment parameters, while 1 SCCM of O2 corresponding to a PO2 = 1.55 × 10−5 mbar, which can be translated into O2-flux of ΦO2 = 4.2 × 1015 cm−2 s−1 by Eq. (6). Consequently, a representing removal efficiency of O2 was obtained according to Eq. (4).
D. Application example
To better illustrate the application scope of our studies, we conducted experimental tests on the device structuring process by in situ Ga-etching a SiO2-masked Ga2O3 layer. Figure 7 showcases the top-view SEM images of the masked and structured Ga2O3 samples. By comparing Fig. 7(a) with Fig. 7(b), as anticipated, we observed Ga droplets remaining on the SiO2 mask after structuring Ga2O3 by exposing it to the Ga flux. However, these droplets can be completely removed in situ by providing O2 following the oxide etching process, as evidenced by a clean mask surface depicted in Fig. 7(c).
IV. SUMMARY AND CONCLUSIONS
In conclusion, we have demonstrated a process in which molecular O2 is utilized to remove elemental Ga and Ge layers in an MBE growth chamber through formation and desorption of their volatile suboxides at temperatures lower than those required for elemental desorption. Under the investigated (nonoptimized) conditions about 1.8%–3.5% of the provided O2 contributed to cation removal.
We further showcased the application of this O2-assisted cation removal process for the in situ removal of the residual Ga droplets from the SiO2 mask directly after structuring a Ga2O3 layer by in situ etching using a Ga atomic flux.
We predict the O2-assisted cation removal process to be generally applicable in situ within an oxide MBE or MOCVD system to remove residual elemental layers (that may occur after exposure to the cation fluxes, e.g., during in situ oxide etching or substrate-temperature calibration) if their volatile suboxides or oxides exhibits a higher vapor pressure than the respective elements, such as B, In, La, Si, Sn, Sb, Mo, Nb, Ru, Ta, V, and W.9,31
The fraction of O2 contributing to cation removal may be increased by using different substrate temperatures from those employed in our experiments to affect activation of suboxide formation or parasitic O2 desorption from the substrate. An increase of the total cation layer removal rate, however, necessitates at some point higher O2-fluxes feeding the suboxide formation and higher substrate temperatures to ensure correspondingly faster suboxide desorption rates. These efficiency and speed aspects provide room for future optimization of the O2-assisted cation removal process, particularly by studying its substrate-temperature dependence.
ACKNOWLEDGMENTS
The authors thank Hans-Peter Schönherr, Claudia Hermann, Sander Rauwerdink, and Walid Anders for technical support, Steffen Breuer for discussion, as well as Jingxuan Kang for critically reading the manuscript. This work was performed in the framework of GraFOx, a Leibniz-ScienceCampus partially funded by the Leibniz association. W.C. gratefully acknowledges financial support from the Leibniz association under Grant No. K417/2021.
AUTHOR DECLARATIONS
Conflicts of Interest
The authors have no conflicts to disclose.
Author Contributions
Wenshan Chen: Formal analysis (equal); Investigation (equal); Visualization (equal); Writing – original draft (equal); Writing – review & editing (equal). Kingsley Egbo: Formal analysis (supporting); Investigation (supporting); Writing – review & editing (supporting). Huaide Zhang: Investigation (supporting); Writing – review & editing (supporting). Andrea Ardenghi: Investigation (supporting); Writing – review & editing (supporting). Oliver Bierwagen: Conceptualization (equal); Funding acquisition (equal); Project administration (equal); Supervision (equal); Writing – review & editing (equal).
DATA AVAILABILITY
The data that support the findings of this study are available from the corresponding author upon reasonable request.